ML19064B220

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Final Report for the Thermal Study to Support a 316(a) Demonstration: Peach Bottom Atomic Power Station Part 1 of 2
ML19064B220
Person / Time
Site: Peach Bottom  Constellation icon.png
Issue date: 02/28/2014
From:
ERM, Normandeau Associates
To:
Exelon Generation Co, Office of Nuclear Reactor Regulation
Hayes B, NRR-DMLR 415-7442
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ML19064B212 List:
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Download: ML19064B220 (199)


Text

FINAL REPORT FOR THE THERMAL STUDY TO SUPPORT A §316(a)

DEMONSTRATION PEACH BOTTOM ATOMIC POWER STATION Prepared for:

Exelon Generation ,.

Prepared by: Normandeau Associates, Inc. and ERM, Inc.

February 2014

Final Report PBAPS Thermal Study Table of Contents Executive Summary .................................................................................................................... 1 1 Introduction ......................................................................................................................... 5 2 Background ......................................................................................................................... 8

2. 1 The Peach Bottom Atomic Power Station .................................................................... 8 2.2 Source Waterbody Description ................................................................................... 11 2.3 Biota of Conowingo Pond............................................................................................ 12 2.4 Summary of Previous 316(a) Demonstration and Important Biological Studies ........... 13 3 Temperature Monitoring Program ...................................................................................... 15
3. 1 Station Descriptions .................................................................................................... 16 3.2 Conditions during the Study Years .............................................................................. 20 3.3 Cooling Tower Performance ....................................................................................... 23 3.4 Effectiveness of Cooling Towers in Reducing Downstream Temperatures .................. 27 3.5 Conclusions ................................................................................................................32 4 Representative Important Species (RIS) ............................................................................ 33 4.1 Bluegill ........................................................................................................................33 4.2 Bluntnose Minnow.......................................................................................................34 4.3 Channel Catfish ..........................................................................................................34 4.4 Gizzard Shad ..............................................................................................................34 4.5 Largemouth Bass........................................................................................................35
4. 6 Chesapeake Logperch ................................................................................................36
4. 7 Smallmouth Bass ........................................................................................................36 4.8 Spotfin Shiner .............................................................................................................37 4.9 Walleye .......................................................................................................................38 4.10 White Crappie .............................................................................................................38 4.11 White Sucker ..............................................................................................................38

Final Report PBAPS Thermal Study 5 Biological Monitoring and Assessment .............................................................................. .40 5.1 lntroduction .................................................................................................................40 5.2 Biological Station Temperatures .............................................................. ................... 40

5. 3 Dissolved Oxygen Conditions ..................................................................................... 54
5. 4 Shoreline Habitat ........................................................................................................ 62
5. 5 Benthic Macroinvertebrate Community ....................................................................... 67
5. 6 Fish Community .............. .......................................................................................... 106
5. 7 Summary and Conclusions ....................................................................................... 226 6 Hydrothermal and Avoidance Modeling .... ...................... ...................... ............................ 230
6. 1 Choice of Hydrothermal Model................ ......................... ......................................... 230
6. 2 Data Needed to Support the Application of the Model ............................................... 232 6.3 Model Calibration ... ...... ... ..... ......... ... ...................................... ... .............. ................ .. 238 6.4

Conclusions:

Hydrothermal Modeling ..................... ................................................... 243

6. 5 Avoidance Model ......................................................................................................243
6. 6 Modeling Scenarios ... ........... ............................ ............................................... .. .. .. .. .244
6. 7 Modeled Thermal Plume for Typical and Extreme Conditions ................................... 252 7 Post-EPU Biological Assessment. ....................................................................................305 7.1 Modeled RIS Avoidance and Benthos Impacts Areas ............................................... 305 7.2 Biological Assessment of Potential RIS Avoidance and Benthos Impact Areas ......... 356 8 Summary of Conclusions .................................................................................................376 9 Glossary .... .. .......................................................................................... .......................... 379 10 Literature Cited ............................................................................................................. 380 10.1 Genera/.....................................................................................................................380 10.2 GEMSS..................................................................................................................... 391 11 Appendices .................................................................................................................. 396
11. 1 Study Plan ................................................................................................................396 ii

Final Report PBAPS Thermal Study

11. 2 Supplemental Data ...................................................................................................396
11. 3 DVD with Model and Results .................................................................................... 396 iii

Final Report PBAPS Thermal Study List of Figures Figure 2-1. Location of Conowingo Pond ................................................................................... 9 Figure 2-2. PBAPS discharge canal with cooling towers locations and designations (circled area is the end of the discharge canal) .............................................................................................. 10 Figure 2-3. PBAPS discharge structure at the end of the canal, looking upstream .................... 11 Figure 3-1. Transect locations and designations ......................................................... ........ .. .... 17 Figure 3-2. Seining station locations and designations ............................................................. . 18 Figure 3-3. Electrofishing station locations and designations . ...... ........... .. .................. ........ .. .... 19 Figure 3-4. PBAPS cooling water system station locations and designations ............................ 20 Figure 3-5. Annual temperature cycle for 2010-2013 and historic (1999-2013) average ......... .. .21 Figure 3-6. Cooling water station data, 2010 ... .... .... .. .. .. ..... .. ............... .. ............... .. .................. .24 Figure 3-7. Cooling water station data, 2011 ............................................................................. 25 Figure 3-8. Cooling water station data, 2012 . ........... .. ............................................................... 25 Figure 3-9. Cooling water station data, 2013 .............................................................................26 Figure 3-10. Transects and stations used in the cooling tower analysis .................................... 30 Figure 5-1. Daily mean water temperature measured at Station 220, 2010-2013 ...................... 43 Figure 5-2. Daily mean water temperature measured at PBAPS Intake, 2010-2013 ................ .43 Figure 5-3. Daily mean water temperature measured at Station 208, 2010-2013 ...................... 44 Figure 5-4. Daily mean water temperature measured at Station 214, 2010-2013 . ........ .. ........... 44 Figure 5-5. Daily mean water temperature measured at Station 215, 2010-2013 ....... .. ............ .45 Figure 5-6. Daily mean water temperature measured at Station 189, 2010-2013 ..................... .45 Figure 5-7. Daily mean water temperature measured at Station 190, 2010-2013 ..... ... .... ....... .. .46 Figure 5-8. Daily mean water temperature measured at Station 216, 2010-2013 ..................... .46 Figure 5-9. Daily mean water temperature measured at Station 217, 2010-2013 ....... .. ............. 47 Figure 5-10. Daily maximum instantaneous water temperature measured at Station 220, 2010-2013 ................................................................................................................... ....................... 47 Figure 5-11 . Daily maximum instantaneous water temperature measured at PBAPS Intake, 2010-2013 ............................... .......................................... ........... ............................................. 48 Figure 5-12. Daily maximum instantaneous water temperature measured at Station 208, 2010-2013 ................................. ......... ............ .................... ......... ............................... ......... ............... 48 iv

Final Report PBAPS Thermal Study Figure 5-13. Daily maximum instantaneous water temperature measured at Station 214, 2010-2013 .. ...... .... .... ....... ........ .. .... ... ..... .............................. ........................... .. ............................. .. ... 49 Figure 5-14. Daily maximum instantaneous water temperature measured at Station 215, 2010-2013 .. ........... .. ................ ................. ... ........ .. ........ .... ................... ... ........ .. ................................. 49 Figure 5-15. Daily maximum instantaneous water temperature measured at Station 189, 2010-2013 .. ......... .............................. .... ...... .......... ... .................. .. ........ .. ........ .. .................................. 50 Figure 5-16. Daily maximum instantaneous water temperature measured at Station 190, 2010-2013 ... ........ ................................................... ............................... .. ....... .................................... 50 Figure 5-17. Daily maximum instantaneous water temperature measured at Station 216, 2010-2013 ..................... ... ........ ................... .. ................... .. ............................................................... .51 Figure 5-18. Daily maximum instantaneous water temperature measured at Station 217, 2010-2013 ..................... ......................................... ... ....... .. .................. .. ........................................... .51 Figure 5-19. Dissolved oxygen measured at the surface and at the bottom at four locations in Conowingo Pond, June to October 1999. Reproduced from Normandeau Associates 2000.... 60 Figure 5-20. Area of shallow shoreline habitat within Conowingo Pond ................................... .. 64 Figure 5-21 . Shallow shoreline habitat in the vicinity of the PBAPS discharge canal. ...... .......... 65 Figure 5-22. Location of seine and benthic macroinvertebrate collection stations........ ......... .... 78 Figure 5-23. Location of electrofishing collection stations .. .. ..................................................... 79 Figure 5-24. Location of trawl collection stations ................................................ .. .... ................. 80 Figure 5-25. Combined map showing locations of seine, benthic macroinvertebrate, and electrofishing collection stations ... ................. ...... .................... ........... .... .... ........... .... .... ..... .... .. .81 Figure 5-26. Box plot illustrating IBI Scores for each benthos station, 2010-2013. (boxes =

interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box= highest and lowest values, and asterisk= outlier) ................... .. 93 Figure 5-27. Box plot illustrating IBI scores for each year by benthos station, 2010-2013. (boxes

= interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box= highest and lowest values, and asterisk= outlier) ......... 93 Figure 5-28. Box plot illustrating IBI scores for each month by benthos station, 2010-2013.

(boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, and asterisk = outlier)

.. ..... ...... .... .. ........ ....... .... ..... .. ........................ .................... ......................................... ............... 94 Figure 5-29. Box plot illustrating total richness for each benthos station, 2010-2013. (boxes =

interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box= highest and lowest values, circle= mean, and asterisk= outlier)

.. .. .................... ........... ......... .. .. ........ .. ...... ..... .... .... ... ...... .............. .. ..... ..... .................... ...... ..... .. 95 Figure 5-30. Box plot illustrating EPT richness for each benthos station, 2010-2013. (boxes =

interquartile range containing 50% of the values, the line across the box = median value, vertical v

Final Report PBAPS Thermal Study lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier)

... ..................................................... ..................... ..... ............. ...... ....... .... ........ ......... ............. ... 95 Figure 5-31. Box plot illustrating Ephemeroptera richness for each benthos station, 2010-2013.

(boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk= outlier) ...................................................................................................................... 96 Figure 5-32. Box plot illustrating Trichoptera richness for each benthos station, 2010-2013.

(boxes = interquartile range containing 50% of the values, the Iine across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk= outlier) .... ...... ... ....... ... ......... ............. .. ........... ............. .. ....................................... ...... 96 Figure 5-33. Box plot illustrating Beck's Index values for each benthos station, 2010-2013.

(boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) .......................................................................... ............................................ 97 Figure 5-34. Box plot illustrating Shannon Diversity values for each benthos station, 2010-2013.

(boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk= outlier) ...... ....... ... .. .... ....... .. ........................ .. ....... .. ................... ... .. ... .........................97 Figure 5-35. Bar chart showing relation of mean IBI scores by year for each benthos station ... 98 Figure 5-36. Box plot illustrating relation of monthly IBI scores for non-thermal (upstream) benthos stations and Stations 214 and 215, 2010-2013. (boxes= interquartile range containing 50% of the values, the fine across the box = median value, vertical Iines extending from the box

highest and lowest values, circle = mean, and asterisk = outlier) ........................................... 99 Figure 5-37. Relation of IBf score and water temperature for Station 215 in 2010 ................... 102 Figure 5-38. Relation of IBl score and water temperature for Station 215 in 2011 ...... ............. 102 Figure 5-39. Relation of IBl score and water temperature for Station 215 in 2012 ................... 103 Figure 5-40. Relation of IBf score and water temperature for Station 215 in 2013 ................. .. 103 Figure 5-41 . Relation of daily mean water temperature and IBI score for Station 215, August-October, 201 O and April-October, 2011-2013 ........................................ .............. .................... 105 Figure 5-42. Box plot of square root transformed CPUE (no./0.5hr) for all electrofishing stations, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical fines extending from the box = highest and lowest values, circle= mean, and asterisk= outlier) ................................................ ...... .. ...... .. .......... 141 Figure 5-43. Box plot of species richness for all boat efectrofishing stations, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box

median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk= outfier) ........................................... .... ................... ... ... ... ......... .............. .. .......... 142 vi

Final Report PBAPS Thermal Study Figure 5-44. Box plot of RIS richness for all boat electrofishing stations, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box =

median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk= outlier) ..............................................................................................................142 Figure 5-45. Box plot of Shannon diversity values for all boat electrofishing stations, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle

mean, and asterisk= outlier) ................................................................................................ 143 Figure 5-46. Box plot of evenness values for all boat electrofishing stations, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box

median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk= outlier) ..............................................................................................................143 Figure 5-47. Box plot of square root transformed CPUE (no./0.5hr) by month for all electrofishing stations, April to October 2010-2013. (4 =April, 5 =May, 6 =June, etc.) (boxes=

interquartile range, line across box = median value, and vertical lines extending from the box =

highest and lowest values) ......................................................................................................144 Figure 5-48. Box plot of species richness by month for all boat electrofishing stations, April to October 2010-2013. (4 =April, 5 =May, 6 =June, etc.) (boxes= interquartile range, line across box= median value, and vertical lines extending from the box= highest and lowest values) .. 144 Figure 5-49. Box plot of RIS richness by month for all boat electrofishing stations, April to October 2010-2013. (4 =April, 5 =May, 6 =June, etc.) (boxes= interquartile range, line across box= median value, and vertical lines extending from the box= highest and lowest values) .. 145 Figure 5-50. Box plot of Shannon diversity by month for all boat electrofishing stations, April to October 2010-2013. (4 =April, 5 =May, 6 =June, etc.) (boxes= interquartile range, line across box= median value, and vertical lines extending from the box= highest and lowest values) .. 145 Figure 5-51. Box plot of evenness by month for all boat electrofishing stations, April to October 2010-2013. (4 =April, 5 = May, 6 =June, etc.) (boxes= interquartile range, line across box=

median value, and vertical lines extending from the box= highest and lowest values) ............ 146 Figure 5-52. Box plot of square root transformed CPUE (no./collection) by station for seine collections, April to October 2010-2013.(boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle= mean, and asterisk= outlier) ......................................................... 154 Figure 5-53. Box plot of fish species richness (no./collection) by station for seine collections, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) ........... .. ............................................................. 155 Figure 5-54. Box plot of RIS richness (no./collection) by station for seine collections, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle

=mean, and asterisk= outlier) ................................................................................................ 155 vii

Final Report PBAPS Thermal Study Figure 5-55. Box plot of Shannon diversity values by station for each monthly seine collection, April to October 2010-2013. (boxes= interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) ... .............. ............ .. ............. ....... ...... .. ...... ... .. .... 156 Figure 5-56. Box plot of evenness values by station for each monthly seine collection, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box= median value, vertical lines extending from the box= highest and lowest values, circle

mean, and asterisk = outlier) ... ...... ... ..... ........ .... .. .. .... ...... .. ... ... .... .... ... ... .. .. ...... .... ... .. .. .. .. ..... .156 Figure 5-57. Box plot of square root transformed CPUE (no./collection) by month for all seine stations, April to October 2010-2013. (4=April, 5=May, 6=June, etc.) (boxes = interquartile range, line across box = median value, and vertical lines extending from the box highest and

lowest values) .... .... ........ ... ... ...... .... ............... ..... ... .. .. ........ .... ........ ... ... .. .. ............. .. ... ..... ... .. .... 159 Figure 5-58. Box plot of species richness by month for all seine stations, April to October 2010-2013. (4=April, 5=May, 6=June, etc.) (boxes = interquartile range, line across box = median value, and vertical lines extending from the box = highest and lowest values) ... .......... ........... 159 Figure 5-59. Box plot of RIS richness by month for all seine stations, April to October 2010-2013. (4=April, 5=May, 6=June, etc.) (boxes = interquartile range, line across box = median value, and vertical lines extending from the box= highest and lowest values) .... .. ....... .. ......... 160 Figure 5-60. Box plot of Shannon diversity values by month for all seine stations, April to October 2010-2013. (4=April, 5=May, 6=June, etc.) (boxes= interquartile range, line across box

= median value, and vertical lines extending from the box = highest and lowest values) ......... 160 Figure 5-61. Box plot of evenness values by month for all seine stations, April to October 2010-2013. (4=April, 5=May, 6=June, etc.) (boxes = interquartile range, line across box = median value, and vertical lines extending from the box= highest and lowest values) ........................ 161 Figure 5-62. Number of Gizzard Shad passed at Conowingo, Holtwood, Safe Harbor, and York Haven Dam, 1997-2011. Data taken from Exelon's annual Cowowingo Dam fish lift reports ... 161 Figure 5-63. Length-frequency distribution of Bluegill collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), July to October 2010.......... ....................... ............ .................................................. 188 Figure 5-64. Length-frequency distribution of Bluegill collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2011 ...................... ........... ................................................... ........ .. 188 Figure 5-65. Length-frequency distribution of Bluegill collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2012 ....... .... ... .... .. .............. ....... ................... .... .... .......... ..... ....... .... 189 Figure 5-66. Length-frequency distribution of Bluegill collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2013 ................................ .................... .......... .. ....... ............. .......... 189 viii

Final Report PBAPS Thermal Study Figure 5-67. Length-frequency distribution of Bluntnose Minnow collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), July to October 2010 .................................................................................... 190 Figure 5-68. Length-frequency distribution of Bluntnose Minnow collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2011 ...................................................................................190 Figure 5-69. Length-frequency distribution of Bluntnose Minnow collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2012 ............................... .................................................... 191 Figure 5-70. Length-frequency distribution of Bluntnose Minnow collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2013 ................................................................................... 191 Figure 5-71. Length-frequency distribution of Channel Catfish collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), July to October 2010... ..................... ............................................................ 192 Figure 5-72. Length-frequency distribution of Channel Catfish collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2011 ................................................................................... 192 Figure 5-73. Length-frequency distribution of Channel Catfish collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2012 ................................................................................... 193 Figure 5-74. Length-frequency distribution of Channel Catfish collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2013 ................................................................................... 193 Figure 5-75. Length-frequency distribution of Gizzard Shad collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), July to October 2010 ........................... ..... ...... ............................................ ..... ........ 194 Figure 5-76. Length-frequency distribution of Gizzard Shad collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2011 .............................................................................................. 194 Figure 5-77. Length-frequency distribution of Gizzard Shad collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2012.. .................. .... ......................................... ............................. 195 Figure 5-78. Length-frequency distribution of Gizzard Shad collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2013 .............................................................................................. 195 Figure 5-79. Length-frequency distribution of Largemouth Bass collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), July to October 2010 . ..................... .................................... .......................... 196 ix

Final Report PBAPS Thermal Study Figure 5-80. Length-frequency distribution of Largemouth Bass collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2011 ................................................................................... 196 Figure 5-81. Length-frequency distribution of Largemouth Bass collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2012 ................................................................................... 197 Figure 5-82. Length-frequency distribution of Largemouth Bass collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2013................................................................................... 197 Figure 5-83. Length-frequency distribution of Chesapeake Logperch collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), July to October 2010 ........................................................................ 198 Figure 5-84. Length-frequency distribution of Chesapeake Logperch collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2011 ...................................................................... 198 Figure 5-85. Length-frequency distribution of Chesapeake Logperch collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2012 ...................................................................... 199 Figure 5-86. Length-frequency distribution of Chesapeake Logperch collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2013 ...................................................................... 199 Figure 5-87. Length-frequency distribution of Smallmouth Bass collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), July to October 2010 ....................................................................................200 Figure 5-88. Length-frequency distribution of Smallmouth Bass collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2011 ...................................................................................200 Figure 5-89. Length-frequency distribution of Smallmouth Bass collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2012...................................................................................201 Figure 5-90. Length-frequency distribution of Smallmouth Bass collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2013 ...................................................................................201 Figure 5-91. Length-frequency distribution of Spotfin Shiner collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), July to October 2010...............................................................................................202 Figure 5-92. Length-frequency distribution of Spotfin Shiner collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2011 ..............................................................................................202 x

Final Report PBAPS Thermal Study Figure 5-93. Length-frequency distribution of Spotfin Shiner collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2012 .............................................................................................. 203 Figure 5-94. Length-frequency distribution of Spotfin Shiner collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2013 ......................................... .. ....................................... .. .......... 203 Figure 5-95. Length-frequency distribution of Walleye collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), July to October 2010 . .......... .......... ... .................. .. ........ .......... ................... .. ... ......... 204 Figure 5-96. Length-frequency distribution of Walleye collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2011 .............................................................................................. 204 Figure 5-97. Length-frequency distribution of Walleye collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2012 ... ............................... ....... .....................................................205 Figure 5-98. Length-frequency distribution of Walleye collected in Conowingo Pond using all gear types for sample stations upstream (non-thermal) and within the PBAPS thermal plume (thermal), June to October 2013 .......................................... ................................................. ... 205 Figure 5-99. Box plot of Bluegill relative weight relative to station, 2010-2013. (boxes =

interquartile range containing 50% of the values, the line across the box median value, circle = =

mean, and the vertical lines extending from the box = highest and lowest values, asterisk =

outlier) ....... ............ .. ........................................................... .................... ............ ......... ......... ...213 Figure 5-100. Box plot of Largemouth Bass relative weight relative to station, 2010-2013. (boxes

=interquartile range containing 50% of the values, the line across the box =median value, circle

mean, and the vertical lines extending from the box =highest and lowest values, asterisk

outlier) ............................. .. ....................................... .......... .. ....... .. .......................................... 213 Figure 5-101 . Box plot of Channel Catfish relative weight relative to station, 2010-2013. (boxes

= interquartile range containing 50% of the values, the line across the box = median value, circle

mean, and the vertical lines extending from the box highest and lowest values, asterisk =

outlier) ................................................................................................................................... ..214 Figure 5-102. Box plot of Smallmouth Bass relative weight relative to station, 2010-2013. (boxes

interquartile range containing 50% of the values, the line across the box median value, circle

mean, and the vertical lines extending from the box highest and lowest values, asterisk =

outlier) ..................................................................................................................................... 214 Figure 5-103. Square root transformed mean CPUE for Bluegill collected using a seine in Conowingo Pond, June-October 1966-2013......................................................................... ..219 Figure 5-104. Square root transforme mean CPUE for Smallmouth Bass collected using a seine in Conowingo Pond, June-October 1966-2013............................................................. ........... 219 xi

Final Report PBAPS Thermal Study Figure 5-105. Square root transformed mean CPUE for Spotfin Shiner collected using a seine in Conowingo Pond, June-October 1966-2013...........................................................................220 Figure 5-106. Square root transformed mean CPUE for Bluntnose Minnow collected using a seine in Conowingo Pond, June-October 1966-2013..............................................................220 Figure 5-107. Square root transformed mean CPUE for Chesapeake Logperch collected using a seine in Conowingo Pond, June-October 1966-2013..............................................................221 Figure 5-108. Square root transformed mean CPUE(no/0.5hr) for Gizzard Shad collected using a boat electrofisher in Conowingo Pond, June-October 1975-2013 ......................................... 222 Figure 5-109. Square root transformed mean CPUE(no/O.Shr) for White Crappie collected using a boat electrofisher in Conowingo Pond, June-October 1975-2013 ......................................... 222 Figure 5-110. Square root transformed mean CPUE(no/0.5hr) for Small mouth Bass collected using a boat electrofisher in Conowingo Pond, June-October 1975-2013............................... 223 Figure 5-111. Square root transformed mean CPUE(no/0.5hr) for Bluegill collected using a boat electrofisher in Conowingo Pond, June-October 1975-2013.................................................... 223 Figure 5-112. Square root transformed mean CPUE(no/0.5hr) for Channel Catfish collected using a boat electrofisher in Conowingo Pond, June-October 1975-2013............................... 224 Figure 5-113. Square root transformed mean CPUE(no/0.5hr) for Chesapeake Logperch collected using a boat electrofisher in Conowingo Pond, June-October 1996-2013................ 224 Figure 5-114. Square root transformed mean CPUE(no/0.5hr) for Walleye collected using a boat electrofisher in Conowingo Pond, June-October 1975-2013.................................................... 225 Figure 6-1. Model grid .............................................................................................................234 Figure 6-2. Model to data comparison of water surface elevations in Conowingo Pond for 2010 .

...............................................................................................................................................241 Figure 6-3. Model to data comparison of water surface elevations in Conowingo Pond for 2011 .

...............................................................................................................................................242 Figure 6-4. Calculated avoidance areas for Spotfin Shiner at the surface on July 10, 2012 ..... 244 Figure 6-5. Muddy Run pumpback and generation cycle showing flow rates; positive values are into Conowingo Pond ..............................................................................................................250 Figure 6-6. Behavior of the thermal plume at the four instances of the Muddy Run pumpback and generation cycle identified in the previous figure .............................................................. 251 Figure 6-7. Location of transects for cross-sectional diagrams................................................ 253 xii

Final Report PBAPS Thermal Study List of Tables Table 3-1. Ranked summer PBAPS intake temperatures. Shaded temperatures exceed period-of-record averages .................................................................................................................... 22 Table 3-2. Monthly average Susquehanna River flow at Holtwood (cfs). Shaded flows are less than 1967-2013 averages .........................................................................................................23 Table 3-3. Summary of temperatures and temperature reductions in the discharge canal; averages for June 15 to September 15 data, when available .................................................... 27 Table 3-4. Downstream surface temperature reductions from the Head of Canal (°F); averages for June 15 to September 15 data, when available ....................................................................29 Table 3-5. Incremental surface temperature reductions as towers are added (°F); averages for June 15 to September 15 data, when available ................................................... ...................... 29 Table 3-6. Incremental temperature reductions at shoreline stations; averages for June 15 to September 15 data, when available .... ... ......... ................................ ............................ ........... ... 31 Table 3-7. Incremental temperature reductions at nearshore stations - surface; averages for June 15 to September 15 data, when available ......................................................................... 31 Table 3-8. Incremental temperature reductions at nearshore stations - bottom; averages for June 15 to September 15 data, when available ......................................................................... 31 Table 3-9. Incremental temperature reductions at cross-river stations - surface ; averages for June 15 to September 15 data, when available ............................... .............................. ............ 32 Table 5-1. Summary of instantaneous maximum and mean water temperature data for multiple locations within Conowingo Pond in 2010 .................................................................................52 Table 5-2. Summary of instantaneous maximum and mean water temperature data for multiple locations within Conowingo Pond in 2011 ................................................................................. 52 Table 5-3. Summary of instantaneous maximum and mean water temperature data for multiple locations within Conowingo Pond in 2012 .. ............................. .. ..... ...... ..... .................. ... ........... 53 Table 5-4. Summary of instantaneous maximum and mean water temperature data for multiple locations within Conowingo Pond in 2013 .................................................................................53 Table 5-5. Dissolved oxygen and water temperature measured during trawl collections in Conowingo Pond, July through October 2010 ............. ..... ... .......... ........................................... .55 Table 5-6. Dissolved oxygen and water temperature measured during trawl collections in Conowingo Pond, April through October 2011 .......................................................................... 56 Table 5-7. Dissolved oxygen and water temperature measured during trawl collections in Conowingo Pond, April through October 2012 .......................................................................... 58 xiii

Final Report PBAPS Thermal Study Table 5-8. Selected weekly DO profiles at transect locations 0N =western area; M =mid-pond; and E = eastern area) in Conowingo Pond, June-October 1999. Reproduced from Normandeau Associates 2000 ........................................................................................................................61 Table 5-9. Amount of shallow shoreline habitat in Conowingo Pond from vicinity of MRPSF downstream to Conowingo Dam ...............................................................................................66 Table 5-10. Amount of shallow shoreline habitat from the end of the PBAPS discharge canal downstream to Station 215 ........................................................................................................66 Table 5-11. Amount of shallow shoreline habitat from Station 215 to Station 189 ..................... 67 Table 5-12. Description of seine and benthos stations in Conowingo Pond (negative values indicate upstream from the discharge canal) .............................................................................82 Table 5-13. Description of trawl transects in Conowingo Pond. (negative values indicate upstream from the discharge canal) ..........................................................................................82 Table 5-14. Description of electrofishing stations in Conowingo Pond. (negative values indicate upstream from the discharge canal) ..........................................................................................83 Table 5-15. Descriptions of benthic macroinvertebrate community metrics ............................... 83 Table 5-16 Habitat assessment scores for the 10 benthos stations ........................................... 84 Table 5-17. Percent composition of common benthic macroinvertebrates (>1%) collected from Conowingo Pond, July-October 2010 ........................................................................................85 Table 5-18. Percent composition of common benthic macroinvertebrates {>1%) collected from Conowingo Pond, April-October 2011 ..... ....... ....................................... .................................... 86 Table 5-19. Percent composition of common benthic macroinvertebrates {>1%) collected from Conowingo Pond, April-October 2012 .......................................................................................87 Table 5-20. Percent composition of common benthic macroinvertebrates {>1 %) collected from Conowingo Pond, April-October 2013 ....................................................................................... 88 Table 5-21. Benthic community composition at Station 214 during July and August, 2010-2012 and July and August 2013 ........................................................... .............................................. 89 Table 5-22. Summary metrics for benthos community, 2010-2013 ............................................ 89 Table 5-23. Mean and median 181 scores for stations within Conowingo Pond, 2010-2013 ....... 90 Table 5-24. Median metric values for benthic macroinvertebrate collection locations in Conowingo Pond, 2010-2013 ....................................................................................................90 Table 5-25. Mean total richness observed by month at each station, 2010-2013 ..................... 91 Table 5-26. Mean EPT richness observed by month at each station, 2010-2013 ..................... 91 Table 5-27. Mean Trichoptera richness observed by month at each station, 2010-2013 .......... 91 Table 5-28. Mean Ephemeroptera richness observed by month at each station, 2010-2013 .... 92 Table 5-29. Mean Shannon diversity values observed by month at each station, 2010-2013 ... 92 xiv

Final Report PBAPS Thermal Study Table 5-30. Mean Beck's Index values observed by month at each station, 2010-2013 ........... 92 Table 5-31. Number of days each year with daily mean water temperature >93°F for all stations, April 1 to October 31 .................. ............................................................................................. 104 Table 5-32. Number of days each year with instantaneous maximum water temperature >94°F for all stations, April 1 to October 31 ....................................................................................... 104 Table 5-33. List of common and scientific names of fishes collected in Conowingo Pond, 2010-2013 ............................................................................................................................. ........... 111 Table 5-34. Number and percent (%) composition of fishes collected by all gear types in Conowingo Pond, July through October 2010. Species in bold are designated as RIS for this study....................................................................................................................................... 112 Table 5-35. Number and percent (%) composition of fishes collected by all gear types in Conowingo Pond, February and April through October 2011 .................................................. 113 Table 5-36. Number and percent (%) composition of fishes collected by all gear types in Conowingo Pond, January, February and April through October 2012 .................................... 114 Table 5-37. Number and percent(%) composition of fishes collected by boat electrofishing and seining in Conowingo Pond, January, March and April through October 2013 ........................ 115 Table 5-38. Trophic designation of common species and RIS collected in Conowingo Pond, 2010-2013. Trophic designation assigned based on Barbour et al. 1999 and Roth et al. 2000 .

............................................................................................................................................... 116 Table 5-39. Summary of fisheries data collected by boat electrofisher, July through October 2010 ...................................................................................... .. ....... .. ....................................... 117 Table 5-40. Summary of fisheries data collected by 10' seine in Conowingo Pond, July through October 2010 ..........................................................................................................................118 Table 5-41. Summary by station of fisheries data collected by 16' Otter Trawl in Conowingo Pond July through October 2010 ............................................................................................. 119 Table 5-42. Summary of fisheries data by station collected by boat electrofisher in February and April through October 2011 ..................................................................................................... 120 Table 5-43. Summary of fisheries data collected by 10' seine in Conowingo Pond, April through October 2011 ..........................................................................................................................121 Table 5-44. Summary by station of fisheries data collected by 16' Otter Trawl in Conowingo Pond April through October 2011 ............................................................................................ 122 Table 5-45. Summary of fisheries data by station collected by boat electrofisher in January, February, and April through October 2012 .................................................................. ............ 123 Table 5-46. Summary of fisheries data collected by 1O' seine in Conowingo Pond, April through October 2012 ..........................................................................................................................124 Table 5-47. Summary by station of fisheries data collected by 16' Otter Trawl in Conowingo Pond April through October 2012 ............................................................................................ 125 xv

Final Report PBAPS Thermal Study Table 5-48. Summary of fisheries data by station collected by boat electrofisher in January, March, and April through October 2013 .................................................................................. 126 Table 5-49. Summary of fisheries data collected by 10' seine in Conowingo Pond, April through October 2013 . ..... ...... .. ............ ............... .... .. ...... .............. ... ...... .... .. ... .. ... .. ....... ..... .... .. ........... .127 Table 5-50. Square root transformed mean and median CPUE (no./0.5hr) for all boat electrofishing stations, April to October 2010-2013 ................................................................. 139 Table 5-51. Mean and median species richness for all boat electrofishing stations, April to October 2010-2013 . ..... ........................... ................................................................................ 139 Table 5-52. Mean and median RIS richness for all boat electrofishing stations, April to October 2010-2013 ............................................................................................................................... 140 Table 5-53. Mean and median Shannon diversity values for all boat electrofishing stations, April to October 2010-2013 ............................................................................................................. 140 Table 5-54. Mean and median evenness for all boat electrofishing stations, April to October 2010-2013 ........................................................................ ....................................................... 141 Table 5-55. Mean electrofishing CPUE (no./0.5hr) by station for Gizzard Shad collected in Conowingo Pond, April to October 2010-2013 ........................................................................ 147 Table 5-56. Mean electrofishing CPUE (no./0.5hr) by station for Spotfin Shiner collected in Conowingo Pond, April to October 2010-2013 ........................................................................ 147 Table 5-57. Mean electrofishing CPUE (no./0.5hr) by station for Bluntnose Minnow collected in Conowingo Pond, April to October 2010-2013 ........................................................................ 147 Table 5-58. Mean electrofishing CPUE (no./0.5hr) by station for Channel Catfish collected in Conowingo Pond, April to October 2010-2013 ........................................................................ 148 Table 5-59. Mean electrofishing CPUE (no./0.5hr) by station for Bluegill collected in Conowingo Pond, April to October 2010-2013 ...................................... ............ ......................................... 148 Table 5-60. Mean electrofishing CPUE (no./0.5hr) by station for Smallmouth Bass collected in Conowingo Pond, April to October 2010-2013 .. ...................................................................... 148 Table 5-61. Mean electrofishing CPUE (no./0.5hr) by station for Largemouth Bass collected in Conowingo Pond, April to October 2010-2013 ... ................. .................................................... 149 Table 5-62. Mean electrofishing CPUE (no./0.5hr) by station for Chesapeake Logperch collected in Conowingo Pond, April to October 2010-2013 ...................................................... 149 Table 5-63. Mean electrofishing CPUE (no./0.5hr) by station for Walleye collected in Conowingo Pond, April to October 2010-2013 ........................................................................ 149 Table 5-64. Square root transformed mean CPUE (no./0.5hr) for all boat electrofishing stations, January- March 2011-2013 ..................................................................................................... 150 Table 5-65. Species richness for all boat electrofishing stations, January- March 2011-2013.150 Table 5-66. RIS richness for all boat electrofishing stations, January- March 2011-2013 ....... 150 xvi

Final Report PBAPS Thermal Study Table 5-67. Shannon diversity values for all boat electrofishing stations, January- March 2011-2013 ........................................................................................................................................151 Table 5-68. Evenness for all boat electrofishing stations, January- March 2011-2013 ............ 151 Table 5-69. Mean CPUE for Gizzard Shad, January-March 2011-2013 ................................. 151 Table 5-70. Square root transformed mean and median CPUE (no/collection) for seine stations, April to October 2010-2013 .....................................................................................................152 Table 5-71. Mean and median species richness for seine stations, April to October 2010-2013 .

............................................................................................................................................... 152 Table 5-72. Mean and median RIS richness for seine stations, April to October 2010-2013 ... 153 Table 5-73. Mean and median Shannon diversity for seine stations, April to October 2010-2013.

...............................................................................................................................................153 Table 5-74. Mean and median evenness for seine stations, April to October 2010-2013 ....... 154 Table 5-75. Mean seine CPUE (no./collection) by station for Spotfin Shiner collected in Conowingo Pond, April to October 2010-2013 ........................................................................ 157 Table 5-76. Mean seine CPUE (no./0.5hr) by station for Bluntnose Minnow collected in Conowingo Pond, April to October 2010-2013 ................................. ....................................... 157 Table 5-77. Mean seine CPUE (no./collection) by station for Bluegill collected in Conowingo Pond, April to October 2010-2013 .................................................................................... ....... 157 Table 5-78. Mean seine CPUE (no./collection) by station for Smallmouth Bass collected in Conowingo Pond, April to October 2010-2013 ......................... ...... ............... .......................... 158 Table 5-79. Mean seine CPUE (no./collection) by station for Chesapeake Logperch collected in Conowingo Pond, April to October 2010-2013 ........................................................................ 158 Table 5-80. Number of each species collected using seine and electrofishing gear across a range of water temperature for non-thermally affected locations within Conowingo Pond, April-October, 2010-2013 ................................................................................................................ 164 Table 5-81. Number of each species collected using seine and electrofishing gear across a range of water temperature for thermally affected locations within Conowingo Pond, April-October, 2010-2013 ................................................................................................................ 165 Table 5-82. CPUE (number/0.5hr) and water temperature for fishes collected with a boat electrofisher at Station 187, July and August 2010-2013 ......................................................... 170 Table 5-83. CPUE (number/0.5hr) and water temperature for fishes collected with a boat electrofisher at Station 164, July and August 2010-2013 ......................................................... 171 Table 5-84. CPUE (number/0.5hr) and water temperature for fishes collected with a boat electrofisher at Station 165, July and August 2010-2013 .. .. ..................................................... 172 Table 5-85. CPUE (number/0.5hr) and water temperature for fishes collected with a boat electrofisher at Station 161, July and August 2010-2013 ......................................................... 173 xvii

Final Report PBAPS Thermal Study Table 5-86. CPUE (number/0.5hr) and water temperature for fishes collected with a boat electrofisher at Station 189, July and August 2010-2013 ................................. ........................ 174 Table 5-87. CPUE (number/0.5hr) and water temperature for fishes collected with a boat electrofisher at Station 190, July and August 2010-2013 .. .. .............. ...................... .... .......... .. .175 Table 5-88. CPUE (number/0.5hr) and water temperature for fishes collected with a boat electrofisher at Station 217, July and August 2010-2013 ................................. ............. ... .. .... .. 176 Table 5-89. CPUE (number/collection) and water temperature for fishes collected with a seine at Station 202, July and August 2010-2013 ............................................................................. 177 Table 5-90. CPUE (number/collection) and water temperature for fishes collected with a seine at Station 203, July and August 2010-2013 ................................................................ ............. 178 Table 5-91. CPUE (number/collection) and water temperature for fishes collected with a seine at Station 220, July and August 2010-2013 .................................................................. ........... 179 Table 5-92. CPUE (number/collection) and water temperature for fishes collected with a seine at Station 221, July and August 2010-2013 ................................................... .............. ............ 180 Table 5-93. CPUE (number/collection) and water temperature for fishes collected with a seine at Station 208, July and August 2010-2013 ........ .. .... ........ ......... ... ........ .. .. .. .... ... .. .. ....... ........... 181 Table 5-94. CPUE (number/collection) and water temperature for fishes collected with a seine at Station 214, July and August 2010-2013 .... .................. .. ........... .. ........................................ 182 Table 5-95. CPUE (number/collection) and water temperature for fishes collected with a seine at Station 215, July and August 2010-2013 ........ ....................................................... .............. 183 Table 5-96. Descriptive statistics for total length of RIS, July to October 2010 ........................ 206 Table 5-97. Descriptive statistics for total length of RIS, June to October 2011 .......................206 Table 5-98. Descriptive statistics for total length of RIS, June to October 2012 .................... ... 207 Table 5-99. Descriptive statistics for total length of RIS, June to October 2013 ...................... 207 Table 5-100. Descriptive statistics for Bluegill relative weight, 2010-2013 ............................... 211 Table 5-101. Descriptive statistics for Largemouth Bass relative weight, 2010-2013 ...............211 Table 5-102. Descriptive statistics for Channel Catfish relative weight, 2010-2013 ..... .. ........ .. 212 Table 5-103. Descriptive statistics for Smallmouth Bass relative weight, 2010-2013 ............... 212 Table 5-104. Total number of each species with DELTS for all gear types and all sample locations in Conowingo Pond, July to October 2010 ................................................................ 216 Table 5-105. Total number of each species with DELTS for all gear types and all sample locations in Conowingo Pond, February to October 2011.. .......................................... ............ 216 Table 5-106. Total number of each species with DELTs for all gear types and all sample locations in Conowingo Pond, January to October 2012... ...... .. ... .. .... .... .. .. .... ...... .... ... ...... .. .... 217 xviii

Final Report PBAPS Thermal Study Table 5-107. Total number of each species with DELTs for all gear types and all sample locations in Conowingo Pond, January to October 2013......................................................... 217 Table 6-1. Mean errors (computed minus observed) by station group for September 2010 ..... 239 Table 6-2. Error statistics and EPA guidance by station group for September 2010 ................ 240 Table 6-3. Numbers of Susquehanna River high temperature and low flow events; the annual probabilities of these events can be obtained by dividing by 20,299 ........................................ 246 Table 6-4. Modeling simulation identifiers and conditions ............................... ......................... 247 Table 6-5. Observed temperature-discharge measurements at Holtwood similar to the extreme summer condition modeling scenario, 2010-2013 ...................................................................248 Table 6-6. Modeled cross-sectional areas (fraction of total, in per cent) exceeding various temperatures for the four cooling tower cases, typical and extreme summer conditions, CLTP

...............................................................................................................................................255 Table 6-7. Modeled areas (acres) exceeding various temperatures for the four cooling tower cases, typical and extreme summer conditions, EPU ..............................................................256 Table 7-1. Modeled cross-sectional areas (fraction of total, in per cent) exceeding various temperatures for the four cooling tower cases, typical and extreme summer conditions, EPU 306 Table 7-2. Modeled areas (acres) exceeding various temperatures for the four cooling tower cases, typical and extreme summer conditions, EPU .............................................................. 307 Table 7-3. Modeled and percent reduction in avoidance area at various water depths for Spotfin Shiner (avoidance temperature= 31°C) based on typical summer scenario (80 °F ambient water temperature and discharge of 13,000 cfs) at EPU for the four cooling tower (CT) cases ......... 369 Table 7-4. Modeled and percent reduction in avoidance area at various water depths for Walleye and White Crappie (avoidance temperature= 32°C) based on typical summer scenario (80 °F ambient water temperature and discharge of 13,000 cfs) at EPU for the four cooling tower (CT) cases ..............................................................................................................................369 Table 7-5. Modeled and percent reduction in avoidance area at various water depths for Smallmouth Bass, Bluntnose Minnow and Gizzard Shad (avoidance temperature = 33°C) based on typical summer scenario (80 °F ambient water temperature and discharge of 13,000 cfs) at EPU for the four cooling tower (CT) cases ..............................................................................370 Table 7-6. Modeled and percent reduction in avoidance area at various water depths for Bluegill, Channel Catfish, and Largemouth Bass (avoidance temperature = 34°C) based on typical summer scenario (80 °F ambient water temperature and discharge of 13,000 cfs) at EPU for the four cooling tower {CT) cases ......................................................................................370 Table 7-7. Modeled and percent reduction in avoidance area at various water depths for Walleye, White Crappie, and White Sucker (avoidance temperature= 32°C) based on extreme summer scenario (86°F ambient water temperature and discharge of 7,000 cfs) at EPU for the four cooling tower {CT) cases .................................................................................................371 xix

Final Report PBAPS Thermal Study Table 7-8. Modeled and percent reduction in avoidance area at various water depths for Smallmouth Bass and Bluntnose Minnow (avoidance temperature = 33°C} based on extreme summer scenario (86°F ambient water temperature and discharge of 7,000 cfs} at EPU for the four cooling tower (CT} cases .................................................................................................371 Table 7-9. Modeled and percent reduction in avoidance area at various water depths for Spotfin Shiner, Gizzard Shad, and Bluegill (avoidance temperature = 35°C} based on extreme summer scenario (86°F ambient water temperature and discharge of 7,000 cfs} at EPU for the four cooling tower (CT} cases ......................... ............................................................................... 372 Table 7-10. Modeled and percent reduction in avoidance area at various water depths for Largemouth Bass (avoidance temperature= 36°C} based on extreme summer scenario (86°F ambient water temperature and discharge of 7,000 cfs} at EPU for the four cooling tower (CT}

cases ......................................................................................................................................372 Table 7-11. Modeled and percent reduction in avoidance area at various water depths for Channel Catfish (avoidance temperature = 37°C} based on extreme summer scenario (86°F ambient water temperature and discharge of 7,000 cfs} at EPU for the four cooling tower (CT}

cases .............................................................................................................. ........................ 373 Table 7-12. Upper avoidance temperatures for RIS based on 30°C (86°F} acclimation temperature. Avoidance temperatures were evaluated based on review of relevant literature.374 Table 7-13 Upper avoidance temperatures for RIS based on 26.7°C (80°F} acclimation temperature ............................................................................................................................375 Table 7-14. Total number of RIS collected at elevated water temperatures, 2010-2013 ......... 375 xx

Final Report PBAPS Thermal Study Executive Summary Exelon's Peach Bottom Atomic Power Station (PBAPS or Station) is a two-unit, power generating station in York County, Pennsylvania. The Station operates under NPDES Permit No. PA0009733 and a Clean Water Act §316(a) variance for its thermal discharge to Conowingo Pond, an impoundment on the Susquehanna River.

This demonstration supports Exelon's request for a thermal variance and represents the culmination of extensive studies and analyses of Conowingo Pond and the Station's operations.

This demonstration shows that the previous thermal variance has assured, and the requested variance will continue to assure, the protection and propagation of a Balanced Indigenous Community (BIC) of aquatic biota in Conowingo Pond, thereby meeting the 316(a) standard for granting a thermal variance.

The biota of Conowingo Pond has been studied for many years, both prior to operation of PBAPS in 1974 and in the subsequent operational period. The most recent prior thermal demonstration study occurred from 1996 to 1999.

This report describes the 4-year thermal study that consisted of fish and benthic macroinvertebrate community sampling and temperature monitoring in Conowingo Pond during periods without cooling towers (in 2010) and when one (2011), two (2012), and three (2013) cooling towers operated. Overall, 224 benthic macroinvertebrate samples were collected at 10 stations. For fish, a total of 673 collections were completed using trawl, seine, and boat electrofisher at 30 stations. Hydrothermal modeling was used to predict thermal plume configurations for Current Licensed Thermal Power (CLTP) and for the increased thermal load that will occur after the pending Extended Power Uprate (EPU). The EPU will increase licensed thermal power and result in a maximum increase in the discharge temperature of 3°F from the existing thermal power level.

Temperature Monitoring Program The objectives of the temperature monitoring program were to:

  • Provide water temperatures at each biological sampling station to support the interpretation of biological data,
  • Obtain temperature data for a range of environmental conditions, and
  • Support the hydrothermal model.

The temperature data under CLTP were used to analyze the changes in the size and configuration of the thermal plume as additional cooling towers were operated. With respect to water temperature reductions from cooling tower operation:

  • The towers performed as designed; each tower cooled the discharge by about an additional 1.6°F, measured from the head to the end of the discharge canal;
  • Operation of the towers reduced water temperatures in Conowingo Pond by consistent and measurable amounts within 1.2 miles of the discharge and near the western shoreline 1

Final Report PBAPS Thermal Study and by smaller amounts beyond 1.2 miles where reductions were variable and related to ambient temperatures and Susquehanna River flows.

Biological Survey The benthic macroinvertebrate survey determined the influence of the thermal plume on the composition and abundance of the benthic community in shallow-water shoreline habitat. The benthic community was evaluated with a PADEP stream assessment protocol. This protocol was used to compare Index of Biotic Integrity scores for all of the sampling stations, both within and outside of the thermally affected areas.

The macroinvertebrate assessment found that there are temperature-related effects on the benthic community; these effects are limited to a narrow band of shallow-water habitat along the western shoreline for a distance no farther than 0.65 miles downstream of the discharge canal.

The temporarily affected area represents approximately 12 acres of the shallow shoreline habitat in Conowingo Pond. Lower 181 scores were only observed during July and August when the thermal plume water temperatures were highest. Improvement in 181 scores occurred in subsequent months indicating re-colonization and recovery of the benthic community.

The spatial and temporal distribution of fish relative to the thermal plume was evaluated by sampling at both thermally and non-thermally influenced locations with three methods of sampling: seining, electrofishing, and bottom trawling. This sampling program was similar to, but more extensive than, the fish community sampling that has been performed periodically in Conowingo Pond for over 40 years.

Fish species distribution and community composition were similar at the non-thermal and thermal stations. No thermally stressed fish were observed. Specific analyses of the fisheries data included evaluation of catch per unit of sampling effort, relation of water temperature to fish occurrence, length-frequency distributions, relative weight, and the occurrence of external anomalies. No substantial differences in these metrics were found between thermally influenced locations and those not influenced by the thermal plume.

The overall conclusions from the fish survey are:

  • The fish community has the ability to sustain itself through cyclical seasonal changes,
  • Numerous prey species are abundant in the fish community,
  • Pollution- or heat-tolerant species do not dominate the fish community,
  • No measurable benefit was observed in terms of fish community composition or relative abundance from reduction in temperature resulting from cooling tower operation, and

Based on the evaluation and comparison of relative abundance data from this study and the comparison to the prior fish sampling data in Conowingo Pond, we can conclude:

  • There is considerable variation in relative abundance over time, 2

Final Report PBAPS Thermal Study

  • Differences in relative abundance during the current study did not appear to be related to differences in water temperature resulting from cooling tower operation,
  • Relative abundance of most Representative Important Species in 2010-2013 was within their historic ranges,
  • Variable year-class strength for some species resulted in a wide range of relative abundances over time, and
  • Changes in fish populations are normal and expected due to naturally variable environmental conditions and historic species introductions.

Operation of variable numbers of cooling towers during the study had no detectable benefit to the integrity of the BIC in Conowingo Pond. Fish and benthic macroinvertebrate community composition and relative abundance were similar among study years. No spatial or temporal patterns were evident in the fish or benthic macroinvertebrate community that can be related to the number of cooling towers that were operating.

This study confirmed the overall conclusion of the most recent prior thermal discharge demonstration study that there is a thriving, balanced fish community in Conowingo Pond under current and previous operating conditions. Similarly, the benthos community, within the constraints of the waterbody, is characteristic of a BIC.

Hydrothermal and Avoidance Modeling The overall objective of hydrothermal modeling was to develop a predictive tool to quantify the horizontal and vertical dimensions of the thermal plume prior to and after Extended Power Uprate (EPU) implementation. Calibration and validation of the model showed that it reproduced the hydrodynamic and thermal structure of the Pond relative to the PBAPS thermal discharge, Muddy Run generation and pumpback, diurnal heating and cooling, and other dynamic input parameters.

The hydrothermal model was coupled to a fish avoidance model that was based on species-specific avoidance temperatures. During the course of the study, the avoidance model was shown to overestimate the areas that fish avoided, that is, individuals of certain RIS were found where measured water temperatures exceeded species-specific avoidance temperatures.

The conclusions from hydrothermal modeling are:

  • For the typical summertime condition, areas of fish avoidance would be small, local, and temporary,
  • For the extreme summertime condition, there would be sizable avoidance areas for several species with most of the elevated water temperatures and avoidance areas at the surface or in the immediate vicinity of the discharge canal,
  • The avoidance model over predicts avoidance areas because fish were collected in locations where water temperatures exceeded their laboratory-derived avoidance temperatures, 3

Final Report PBAPS Thermal Study

  • No habitat critical to the maintenance of the SIC would be avoided within the thermal plume, thus diminished maintenance of RIS would not be expected, and
  • Cross-sections of the thermal plume indicate that sufficient areas of the channel will be available at water temperatures less than the avoidance temperatures for the RIS to allow their movement within the Pond.

Overall Conclusions of the Study This demonstration study concludes that under current operation of PBAPS, a SIC exists in Conowingo Pond. This community is characterized by diversity, the capacity to sustain itself through cyclic seasonal changes, and the presence of necessary food chain species; furthermore, the community is not dominated by pollution tolerant species. These characteristics are sufficient for the issuance of a thermal variance as described in USEPA guidance (1977).

There will be a 3°F increase in the discharge temperature after EPU. Based on information from the hydrothermal and avoidance models, as well as biological and temperature data obtained in this study, a SIC will be maintained after the EPU.

The previous 316(a) thermal variance issued in 2000 is appropriate and achieves the goal of protecting and maintaining the SIC. Continuation of the previous thermal variance is appropriate and warranted based on the results of this study. A similar conclusion was reached after the completion of the most recent historic thermal effects study. Consideration should be given to thermal and biological monitoring after the power uprates. Monitoring and evaluation of actual thermal conditions, post-EPU, could be used to determine whether modification from operating under the previous thermal variance is required to maintain a SIC.

4

Final Report PBAPS Thermal Study 1 Introduction Exelon Generation, LLC's (Exelon) Peach Bottom Atomic Power Station's (PBAPS or "the Station") is an electric nuclear power generating facility located in York County, Pennsylvania.

The Station operates under National Pollutant Discharge Elimination System (NPDES) Permit No. PA0009733 and a Federal Clean Water Act (CWA) §316(a) variance for its thermal discharge to Conowingo Pond (the Pond or Conowingo Reservoir) of the Susquehanna River.

As required by the Permit, Exelon conducted a 316(a) Demonstration study, Thermal Study", in 2010 - 2013 for these purposes:

1. As a demonstration study of an alternative thermal effluent limitation (as required by Footnote 3 in Part A of the NPDES permit) and alternative thermal effluent limitations under §316(a) of the CWA,
2. To evaluate changes in the thermal plume created by operation of up to three helper cooling towers, and
3. As a predictive study of the changes to the thermal discharge associated with planned power uprates to Units 2 and 3 of the Station, and predicting the effects of operating helper cooling towers.

A work plan (or study plan) for the thermal study was developed through extensive coordination with the Pennsylvania Department of Environmental Protection (PADEP). The study plan is provided in Appendix 11.1. Sufficient agreement between Exelon and the PADEP was reached on the various technical data collection objectives and methods to begin the field study in July 201 O in advance of the January 2011 effective date of the renewed NPDES permit.

The main components of the study include temperature monitoring and modeling and biological sampling of shore zone benthic macroinvertebrates and the resident fish community throughout the Pond. Field data collection was primarily performed in April through October, the main period of fish reproduction and growth as well as highest ambient and discharge water temperatures. The period of warmest water temperatures, July and August, is emphasized in this report due to PADEP's expressed interest in the potential extent of fish exclusion from habitats affected by the thermal plume. Data collection began in July 2010 and was originally planned to extend through a fifth year, 2014, but the field study was curtailed in 2013, with PADEP concurrence, to accommodate application for a revised NPDES permit due to planned implementation of the extended power uprates (EPU) for Units 2 and 3 starting in 2014.

To support a thermal variance the permittee must demonstrate that the otherwise applicable water quality standard for temperature is more stringent than necessary to assure the protection and propagation of the waterbody's balanced indigenous community or SIC (EPA 2008).

Maintenance of a SIC of aquatic life in the waterbody receiving the thermal discharge is the major requirement for a power station to receive a thermal discharge variance, according to applicable Section 316(a) technical guidance issued by the US Environmental Protection Agency (USEPA 1977). USEPA guidance describes a SIC as a biotic community that:

  • Is typically characterized by diversity,
  • Displays the capacity to sustain itself through cyclic seasonal changes, 5

Final Report PBAPS Thermal Study

  • Includes the presence of necessary food chain species, and
  • Lacks domination by pollution tolerant species.

A BIC may include:

  • Historically non-native species introduced through a program of wildlife management.

This would include several of the non-native RIS (e.g. Smallmouth Bass, Largemouth Bass, etc.) that are now naturalized and a main component of the Susquehanna River fish community. Importantly, the guidance indicates that a BIC can reflect impoundment or other conditions that are essentially irreversible.

  • Species whose presence or abundance results from substantial irreversible environmental modifications unrelated to the thermal discharge.

A BIC will not include:

  • Species whose presence or abundance is attributable to the introduction of pollutants that will be eliminated by having all sources comply with the applicable thermal limits.
  • Species whose presence or abundance is attributable to alternative effluent limitations imposed pursuant to Section 316(a).

An important component of a 316(a) variance is the ability of the discharger to demonstrate the absence of prior appreciable harm to the BIC from the thermal discharge. Key considerations for evaluating appreciable harm were provided in USEPA's 1975 guidance document (USEPA 1975) and include:

  • Substantial increase in abundance or distribution of any nuisance species or heat tolerant community not representative of the highest community development achievable in receiving waters of comparable quality,
  • Substantial decrease in formerly indigenous species, other than nuisance species,
  • Changes in community structure to resemble a simpler successional stage than is natural for the locality and season in question,
  • Unaesthetic appearance, odor or taste of the waters,
  • Elimination of an established or potential economic or recreational use of the waters,
  • Reduction in completion of life cycles of indigenous species, including migratory species, and
  • Substantial reduction in community heterogeneity or trophic structure.

Interim results for the first 3 years of the study; 2010, 2011, and 2012; were reported in Normandeau Associates and ERM (2011, 2012, and 2013a). This final 316(a) thermal variance demonstration report describes the work performed and results for the entire 4-year period of the thermal study. This report presents both retrospective and prospective analyses which show that the thermal variance under which PBAPS operated since 2000 has supported a BIC in Conowingo Pond and the requested thermal variance needed after the power uprates will assure the protection and propagation of a balanced indigenous community (BIC) of aquatic life in the Conowingo Pond, thereby meeting the 316(a) standard for granting of a thermal variance.

6

Final Report PBAPS Thermal Study Section 2 of this demonstration report provides information about PBAPS, Conowingo Pond and previous important thermal effects biological studies conducted relative to PBAPS that will be useful for interpreting the results of the current study. The Representative Important Species of fish that are emphasized in the thermal effects evaluations are discussed in Section 4. The three major components of the demonstration study: biological monitoring, temperature modeling, and hydrothermal modeling; are discussed in Sections 3, 5, and 6, respectively.

Section 7 provides the prospective biological evaluation of potential thermal effects after implementation of the power uprates. A comprehensive summary of conclusions for both the retrospective and prospective evaluations is presented in Section 8. Additional supporting information is provided in Sections 9 (Glossary) and 1O (Literature Cited) and in the Appendices.

This report and the associated study were designed to determine whether there is a SIC within Conowingo Pond.

7

Final Report PBAPS Thermal Study 2 Background This section provides key information about PBAPS and Conowingo Pond as well as a brief summary of the previous 316(a) variance demonstration and the recent biological studies conducted in the Pond relative to the PBAPS thermal discharge.

2. 1 The Peach Bottom Atomic Power Station PBAPS is in York County, Pennsylvania, on the west shore of Conowingo Pond, the lowermost impoundment on the Susquehanna River (Figure 2-1). The Station is located at approximately river mile (RM) 17, about 3 miles upstream from the Pennsylvania-Maryland border and 7 miles upriver from Conowingo Dam. The Station consists of two boiling water reactors and operates as a base-load facility with both units normally generating at full capacity. Unit 2 began commercial operation in June 1974 and Unit 3 entered commercial service in December 1974.

A refueling outage for one of the two units takes place each fall during which one of the units is brought off-line (Unit 2 outages are in even-numbered years, Unit 3 outages are in odd-numbered years). Refueling is preceded by a power coast-down due to nuclear fuel depletion which occurs approximately 6 weeks prior to the start of the refueling outage.

PBAPS withdraws water for condenser cooling and service needs from Conowingo Pond through an outer intake structure, through two 3-acre intake ponds (one pond serving each unit),

and then through an inner intake structure. There are six circulating water pumps (three per unit) that supply cooling water to the condensers and six service water pumps (three per unit) that provide water for process and equipment needs. Each circulating water pump has a nominal capacity of 250,000 gallons per minute (gpm), or 557 cubic feet per second (cfs). Each service water pump has a nominal capacity of 14,000 gpm, or 31.2 cfs. In the winter, some heated water is recirculated from the discharge basin through a small gate that connects to the intake pond, which provides freeze protection for the water supply of the cooling water intakes.

The design temperature rise across the condensers is 22°F and across the service water system is 10.?°F. As noted in Section 3.2, the actual temperature rise for the combined condenser and service water flow as observed in this study averaged 19.4°F at the head of the discharge canal during the two warmest months of the year, July and August.

The heated effluent is discharged into a common discharge basin that leads to a 4,700-ft long discharge canal (Figure 2-2) separated from Conowingo Pond by a berm. The canal terminates downstream (south) of PBAPS at a submerged jet discharge structure (Figure 2-3) designed for rapid mixing of the heated effluent into ambient Conowingo Pond water and immediate reduction in temperature.

8

Final Report PBAPS Thermal Study J

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/ordnance SuNey. Esri Japan METI Esn Chino (Hong Kong) swisstopo Ii and the GIS User Community Figure 2-1. Location of Conowingo Pond.

9

Final Report PBAPS Thermal Study Figure 2-2. PBAPS discharge canal with cooling towers locations and designations (circled area is the end of the discharge canal).

  • 10

Final Report PBAPS Thermal Study Figure 2-3. PBAPS discharge structure at the end of the canal, looking upstream.

2. 2 Source Waterbody Description Conowingo Pond, the lowermost of four hydroelectric impoundments on the lower Susquehanna River, was formed in 1928 by construction of Conowingo Hydroelectric Station at River Mile (RM} 10. Conowingo Hydroelectric Station is a modified run-of-river facility with limited storage for peaking hydropower generation. Conowingo Pond is bounded upstream by Holtwood Dam (RM 24) built in 1914. PBAPS at RM 17 is about equidistant between the two dams.

Conowingo Pond has a surface area of about 9,000 acres and has a design storage capacity of 310,000 acre-ft. It is about 14 miles long and averages 1 mile wide. The elevation at normal full Pond is 108.5 ft (Conowingo Datum} and Pond elevation is normally maintained at 106.5 ft or higher for recreational use on weekends between Memorial Day and Labor Day and at levels no less than 104.5 ft at other times for operation of PBAPS.

Since environmental monitoring began in 1966, there has been no substantial thermal stratification in Conowingo Pond. However, during summer, generally at water temperatures exceeding 75°F and Susquehanna River flows less than 12,000 cfs, dissolved oxygen stratification can occur, particularly in deeper areas of the lower third of the Pond. However, this stratification quickly breaks down during periods of heavy rain and high winds (Mathur et al.

1988). There is no information showing that the temporary dissolved oxygen stratification is caused or influenced by PBAPS. Whaley (1960) showed that dissolved oxygen stratification 11

Final Report PBAPS Thermal Study occurred in the Pond prior to operation of PBAPS; a natural phenomenon for this type of waterbody.

The circulation in the Pond is influenced by outflows and inflows that can occur on a daily or hourly basis from controlled inflows of up to 32,000 cfs from Holtwood Hydroelectric Dam and up to 32,000 cfs (during generation) from Muddy Run Pumped Storage Facility (MRPSF) at RM

22. Controlled outflows of up to 85,000 cfs occur at Conowingo Hydroelectric Station and of up to 28,000 cfs (during pumping) at MRPSF. Conowingo Hydroelectric Station currently has to comply with Federal Energy Regulatory Commission-mandated seasonally adjusted minimum flow requirements.

2.3 Biota of Conowingo Pond The biota of Conowingo Pond has been studied intensely for many years. Long-term thermal and biological monitoring studies have been completed in Conowingo Pond since 1966, both prior to operation of PBAPS in 1974 and in the subsequent operational period. Sampling has been performed upstream and downstream from PBAPS and in areas within the heated plume.

The numerous long-term studies documented species composition, relative abundance and distribution of fishes within Conowingo Pond. The most recent thermal demonstration studies prior to the current 316(a) demonstration study were completed from 1996 to 2000. These studies included thermal profiling and extensive fish community monitoring to examine the potential to reduce the number of cooling towers needed to maintain the integrity of a BIC in Conowingo Pond.

Conowingo Pond is a dynamic and complex biological system in which there is an almost continuous movement of fish and water into and out of the Pond. The complexity of the fish community derives from these three sources:

  • Seasonal immigration into Conowingo Pond from below Conowingo Dam via the East Fish Lift and from above Conowingo Pond through Holtwood Dam,
  • Emigration out of Conowingo Pond via Conowingo Dam and the Holtwood Fish Lift, and

Except for the known number of fish that are transported through the fishways at Conowingo and Holtwood, it is difficult to quantify the recruitment into and losses out of Conowingo Pond.

Extensive sampling throughout Conowingo Pond since the mid-1960s provides substantial historical information concerning the biota (PECO 1975, 1976; Normandeau Associates 1997-2000a).

Water quality standards applicable to Conowingo Pond aquatic life are designated for the protection of warm water fishes and migratory fishes per 25 Pa. Code 93.3. Since 1966, approximately 60 species have been captured in the Pond and the tributary streams. The Comely Shiner, Spotfin Shiner, Bluegill, Green Sunfish, Bluntnose Minnow, and Spottail Shiner are the common forage species. The Channel Catfish is one of the most numerous large-bodied fishes and a target species for some anglers. The Flathead Catfish, a predatory species, was introduced into Conowingo Pond in 2000 and has become widely distributed in the Pond and is sought after by anglers. White Crappie, once abundant through the early 1980's, is now 12

Final Report PBAPS Thermal Study uncommon due to introduction of Gizzard Shad. The common game fishes are the Smallmouth Bass, Largemouth Bass, and, to a lesser extent, Walleye. The RIS members of the fish community are discussed in Section 4.

The distribution of the fish community is not uniform in the Pond. Some species, such as Largemouth Bass, are more common in the lower part of the Pond whereas Smallmouth Bass, Walleye, and Bluntnose Minnow are more common in the upper reaches of the Pond. The Gizzard Shad population, inadvertently introduced in 1972 from below Conowingo Dam, has exploded and this species competes for food with other fishes in the Pond. Large fluctuations in abundance of the common species between sampled locations and years have been well documented (Robbins and Mathur 1976; Normandeau Associates 2000a).

2.4 Summary of Previous 316(a) Demonstration and Important Biological Studies The original 316(a) Demonstration Report, Materials Prepared for the Environmental Protection Agency, 316(a) Demonstration for PBAPS Units No. 2 & 3 on Conowingo Pond (PECO 1975) was submitted to the Pennsylvania Department of Environmental Resources (PADER), now PADEP, and the USEPA in July 1975. This report was submitted by Philadelphia Electric Company, which later changed its name to PECO Energy Company, and subsequently became an Exelon company in 2000. The original 316(a) demonstration sought thermal effluent limitations that were less stringent than would be produced by a closed cycle-cooling system, but yet sufficient to ensure the protection and propagation of a BIC of shellfishes, fishes, and wildlife in and on Conowingo Pond.

The limitations were based on a design consisting of an open-cycle cooling system that used three mechanical draft "helper" cooling towers, cooling 58 percent of the flow that was mixed with the remaining 42 percent of the flow prior to being discharged, via the submerged jet discharge, to the Pond.

In February 1976, the USEPA requested that ecological data in the July 1975 submittal be integrated with predicted isotherms to illustrate the impact of the thermal discharge on biological communities. It was also requested that tables and graphs be used to present the effects of the predicted isotherms on the various life history stages and parameters in the representative important species (RIS) of biota selected by the USEPA for use in the 316(a) demonstration (Elder et al. 1973). Subsequent to the original 316(a) demonstration, evaluation of the potential biological impacts of the thermal discharge focused solely on the fish community because RIS of fish were judged to be representative of the BIC of aquatic biota.

In June 1976, PECO submitted a supplementary report to the agencies documenting the results of this analysis (PECO 1976). This document, entitled Supplementary Materials Prepared for the Environmental Protection Agency, 316(a) Demonstration for PBAPS Units No. 2 & 3 on Conowingo Pond, also stated that the Company agreed to new requirements that included the use of two additional helper towers. The five towers would be operated in a phased manner, from zero to all five towers in operation.

13

Final Report PBAPS Thermal Study In 1977, the agencies approved the phased operation of the cooling towers (zero to five) based on evaluation of ambient water temperature, fish tolerances to sudden change in temperature, and cooling efficiency of the towers (PECO 1977).

From 1996 through 1999, PECO performed a 4-year fishery and habitat avoidance study with zero to two towers in operation to further evaluate the necessity of cooling the heated discharge (Normandeau Associates 1997, 1998, 1999, 2000a, and 2000b). The results of the study indicated that the operation of cooling towers was only needed during certain infrequent concurrent low flow and high water temperature conditions. The regulators (PADEP, Pennsylvania Fish and Boat Commission and Maryland Department of Natural Resources) concurred and the PBAPS heated effluent was thereafter discharged into the Pond without auxiliary cooling. A condition was imposed that required auxiliary cooling with one to two towers under extreme low flow - high water temperature conditions if the fish community showed signs of thermal stress.

To assess thermal-related fish stress and determine if any cooling towers should be operated, the agencies required that a boat-based fish surveillance program be implemented when Susquehanna River flow was less than 3,000 cfs at the Marietta USGS gage and incoming ambient water temperatures at Holtwood Dam were greater than 85°F. Of particular interest was potential stress to the large number of fish (often more than 700,000) introduced annually into Conowingo Pond via the Conowingo East Fish Lift since 1997.

PBAPS operated in this manner, without the need to operate cooling towers at any time or without evidence of fish stress, until 2011 when, during the course of the current 316(a) demonstration study, the PADEP required the use of one or more cooling towers from June 15 through September 15 in 2011 (one cooling tower), 2012 (two cooling towers), and 2013 (three cooling towers).

As noted in the following section, no migratory fish, such as American Shad (Alosa sapidissima) or American Eel (Anguilla rostrata), are included as RIS for this demonstration and, therefore, are not evaluated in this report with regard to interaction with the thermal plume from PBAPS.

However, upstream and downstream passage of American Shad and American Eel were evaluated considering interaction of MRPSF operations and the PBAPS thermal plume at current licensed thermal load by Normandeau Associates and Gomez and Sullivan (2012) and at the greater predicted thermal load post-EPU by Normandeau Associates and ERM (2013b).

Both evaluations found that, among a host of factors, spikes in natural river flows causing spillage >25,000 cubic feet per second at Holtwood Dam with high turbulence, velocities, and turbidity together with inefficient passage at the existing fish passage facilities pose greater impedance to American Shad migration and restoration than operation of either PBAPS or MRPSF individually or together. Radio tagging studies of American Shad showed no evidence of adverse effects of the thermal plume on upstream or downstream migration. Both prior studies indicate that there is no thermal blockage to migratory fishes in Conowingo Pond.

14

Final Report PBAPS Thermal Study 3 Temperature Monitoring Program The four objectives of the temperature monitoring program were to

  • Measure temperatures at the biological sampling stations;
  • Provide a temperature dataset for a range of Holtwood, Muddy Run, PBAPS, and Conowingo operations; and
  • Support calibration and validation of the predictive hydrothermal model.

Data from the monitoring program were also used to determine the effectiveness of cooling towers on reducing temperatures in the discharge canal and downstream of the discharge canal.

This section of the report describes the temperature monitoring system and presents an analysis of the in-canal cooling tower performance as well as a data-based assessment of the towers' effectiveness in reducing temperatures downstream of the discharge canal. Section 6.3 discusses the use of the data to support the model calibration and validation and Section 6.4 describes use of the data for the biological assessment.

As used in this report, a monitor is a single temperature recording instrument, sometimes referred to as a thermistor. A station consists of one or more monitors on a mooring at a specific location. A transect refers to line of stations across or down Conowingo Pond. One set of monitors recorded temperatures of the cooling water system, including cooling tower cold and hot water side temperatures. A second set of monitors recorded temperatures in Conowingo Pond at transects used in previous studies (the "historical transects") and one new transect, and at seining and electrofishing stations.

Thirty-five stations were fitted with one or more monitors. For deep water stations, monitors were placed in a surface-to-bottom configuration, with the number of monitors and their vertical spacing dependent on the water depth at that location. The locations of all stations were logged with a Global Positioning System (GPS) at the time of deployment.

Temperature data for the transect, seining, and electrofishing stations were collected using Onset HOBO Pro v2 Water Temperature Data Loggers. These instruments are accurate to 0.36°F in the range 32 to 122°F, can resolve temperatures to 0.04°F at 77°F, and have a 5-minute response time. Each monitor recorded temperature every 15 minutes. Data from each instrument were downloaded at approximately 4-week intervals. Cooling water station data were collected by a separate set of monitors.

Temperature data were recovered for

  • June 29 to November 29, 201 O;
  • April 1 to December 8, 2011;
  • March 21 to November 14, 2012; and
  • March 22 to November 18, 2013.

15

Final Report PBAPS Thermal Study The monitoring program collected 1.15 million data points in 2010, 1.94 million in 2011, 2.08 million in 2012, and 2.04 million in 2013. In 2011 the passage of Tropical Storm Lee resulted in the temporary loss of several thermistors, which were subsequently replaced.

3. 1 Station Descriptions Thermal monitors were placed along historical Transects 100, 200, 300, 400 and at a single location mid-channel near Hopkins Cove (Station 611 ), for a total of 20 stations. An additional transect was established immediately offshore of the intake (Transect 150) and consisted of three stations. Locations are shown in Figure 3-1. Transects are defined as a series of cross-Pond stations, e.g., Transect 100 includes Stations 101, 102 and 103; Transect 200 includes 201, 202, 203, 204 and 205. Stations along transect 400 were re-located, as requested by DEP, to coincide with historical locations. For most stations, temperatures were measured near-surface (i.e., within 1 ft of the surface), at 5-ft and 10-ft depths, and near-bottom (within approximately 1 ft of the bottom). At the two deeper stations (Stations 402 and 611) temperatures were measured near-surface, at 10-ft and 20-ft depths, and near-bottom.

In addition to the array of monitors shown in Figure 3-1, monitors were installed at eleven seining and electrofishing stations to characterize the temperature history of the biological sampling stations. The seining stations are shown in Figure 3-2 and the electrofishing stations are shown in Figure 3-3. A total of seven monitors were deployed at the seining stations in 2010 (increased to nine in 2011 with the addition of Stations 216 and 217) and at two of the electrofishing Stations (189 and 190). For these stations, the thermal monitors were placed on the bottom in shallow shoreline locations that were less than 5 ft deep.

Additional temperature monitors were deployed to record temperatures from the intake through the end of the discharge canal. Four stations were established to monitor temperatures at the outer and inner intake structures, at the head of the discharge canal, at the exit from the discharge canal and at the inlet and outlet for each operating cooling tower. Figure 3-4 shows the locations of the cooling water stations.

Data collected at cooling water stations allowed calculation of temperature changes

  • from the intake to the discharge at the head of the canal,
  • from the intake to the end of the discharge canal.

Data from these monitors were compared to data from the Conowingo Pond monitors downstream of the discharge to assess the effectiveness of the towers in reducing temperatures downstream of the discharge.

16

Final Report PBAPS Thermal Study Holtwood Dam Muddy Run Station Boat Launch 10l"' Fishing Creek Muddy Creek 101...

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Hopkins Cove t 17

Final Report PBAPS Thermal Study

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18

Final Report PBAPS Thermal Study Holtwood Dam Muddy Run Station Boat Launch Fishing Creek Muddy Creek Rollins Point ~11 Mt. Johnson Island 1£4 l

Peach Bottom Atomic Power \ Peters Creek

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Figure 3-3. Electrofishing station locations and designations.

19

Final Report PBAPS Thermal Study Figure 3-4. PBAPS cooling water system station locations and designations.

3.2 Conditions during the Study Years The behavior of the thermal plume is determined primarily by the PBAPS discharge rate and temperature rise and the Susquehanna River flow rate. Muddy Run pumpback and generation flows and upstream temperatures (an indication of natural heating and cooling due to surface heat exchange) are also important factors, although their effects are primarily in the far-field.

Variations in these forcing functions over the study years are described below.

With the exception of end-of-the summer refueling outages, PBAPS operations were steady for all four study years with a discharge rate of 3,529 cfs (the sum of condenser cooling and service water flows). Unit 2 was shut down for refueling on September 12, 2010 and again on September 9, 2012. Unit 3 was shut down for refueling on September 11, 2011 and on September 9, 2013. Outages last approximately 6 weeks and are preceded by a power coast down which decreases power output and reduces circulating water temperature rises.

To characterize Susquehanna River temperatures during the study period, monthly average PBAPS intake temperatures 201 O through 2013 were compared with long-term records at the PBAPS intake and at Holtwood Dam. Both these records are important. The longer Holtwood Dam record was used to generate the joint flow-temperature distribution discussed in Section 20

Final Report PBAPS Thermal Study 6.6. The shorter PBAPS intake temperature record better represents temperatures in the lower portion of Conowingo Pond.

Temperatures during the study years can be characterized by examining Figure 3-5 which shows the PBAPS monthly-average intake temperatures for the study years as well as period-of-record values. The period-of-record averages are based on hourly temperatures measured at the Unit 2 and Unit 3 intakes for 1999 through October 2013 (a 15-year record). The figure shows a typical northern hemisphere seasonal cycle with the highest temperatures in July and August and a rapid drop-off in September and October.

Table 3-1 shows these same temperatures ranked relative to the period-of-record temperatures.

The months of July and August of 2010 and 2012 stand out as the warmest of the study period and also warm relative to period-of-record averages. August 2013 was notable for low temperatures.

Monthly Averaged Intake Temperature

......... historic (1999-2013)

I

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  • 40

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Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Figure 3-5. Annual temperature cycle for 2010-2013 and historic (1999-2013) average.

21

Final Report PBAPS Thermal Study Table 3-1. Ranked summer PBAPS intake temperatures. Shaded temperatures exceed period-of-record averages.

June Temp, F July Temp, F August Temp, F September Temp, F 2010 78.8 2010 84.0 2010 82.3 2010 75.1 2011 76.2 2012 83.8 2012 81.8 2012 74.2 PBAPS II intake, 2013 75.1 2011 83.3 80.6 2013 73.8 1999-II 2013 Holtwood, Holtwood, 2012 75.0 2013 81.2 1967- 80.2 73.6 1967-2011 2012 PBAPS PBAPS PBAPS intake, intake, 74.8 81 .1 2011 80.1 intake, 1999- 73.1 1999- 1999-2013 2013 2013 Holtwood, Holtwood, 1967- 74.7 1967- 80.6 2013 77.2 2011 68.1 2012 2012 Monthly average Susquehanna River flows were calculated from data available at Holtwood Dam from October 1967 through September 2012 (a 45-year record). The Holtwood Dam flow records were provided by PPL and consist of the sum of flows for the Susquehanna River (at Marietta), Conestoga Creek, and Pequea Creek. These records are continuous from 1967 onwards; prior to 1967 there are long periods without data. To characterize flows in the study years, monthly average flows for April through October in each of the study years were compared to 1967-2012 monthly averages (Table 3-2). Each of these years show typical spring high flows followed by decreased summer flow and a return to higher flows in the fall.

Superimposed on this pattern are large rainfall events, especially in the Spring of 2011, May of 2012, and the Fall of 2011 when Tropical Storm Lee caused flooding in September. Flows peaked at 632,400 cfs at Holtwood on September 9, 2011 during Tropical Storm Lee.

Monthly flows 2010 through 2013 were both above and below the period-of-record averages with below average flows for most of the summer months in 2010 and 2012. August and September 2010 and July 2012 each had average flows less than 10,000 cfs.

22

Final Report PBAPS Thermal Study Table 3-2. Monthly average Susquehanna River flow at Holtwood (cfs). Shaded flows are less than 1967-2013 averages.

Month 1967-2013 2010 2011 2012 2013 April 78,600 46,385 149,867 23,704 53,462 May 48,500 34,392 110,399 52,547 29,717 June 28,900 17,508 35,079 29,693 31,949 July 16,200 10,060 13,202 8,730 37, 117 August 12,700 8,808 17,797 10,275 15,692 September 15,800 6,142 141,479 11,222 12,266 October 18,800 40,228 80,023 18,378 18,853 Overall, the study years covered a representative range of flow and temperature conditions relative to period-of-record values. The summers of 2010 and 2012 represent especially warm temperatures combined with low flows and are ideal periods to collect and analyze data to perform the present study.

3.3 Cooling Tower Performance A key feature of the Study Plan was the sequential operation of an increasing number of cooling towers from June 15 to September 15 each year. Exelon added one cooling tower each year as the study proceeded:

  • 2010- no towers;

The primary heat loss process in a cooling tower is evaporative cooling (approximately 75% of the total heat loss). The remainder of the heat loss is dependent on the temperature of the water supplied to the cooling tower. Cooling tower performance is quoted in terms of an approach temperature, i.e., how closely the cold side temperature "approaches" the ambient wet bulb temperature. The approach temperature conveniently summarizes all heat transfer processes.

Figure 3-6 shows measurements obtained in 2010 when no towers were operating. The shortened period of temperature measurement was the result of later-than-planned installation of monitors. The figure shows temperatures measured at the intake, head, and end of the discharge canal. The difference between the head of the canal and intake temperature is the temperature rise through the plant, an average of 19.2°F for 2010. Water passing through the canal is cooled, on average, by 0.2°F through surface heat loss to the atmosphere for a net change from the intake to the end of the canal of 19.0°F. Note that Unit 2 was shut down for about 6 weeks for refueling on September 12, 2010 Cooling Tower 8 was put into operation on June 13, 2011. Figure 3-7 shows the temperatures at the three stations for June 15 through September 15 of that year. The average temperature rise through P8APS was 19.3°F for this period; the operation of Cooling Tower 8 resulted in net 23

Final Report PBAPS Thermal Study cooling in the canal of 1.9°F and a net change from the intake to the end of the canal of 17.4 °F.

Unit 3 was shut down for refueling on September 11, 2011.

Figure 3-8 shows temperature measurements for 2012 when two cooling towers operated. The average temperature rise through PBAPS was 19.0°F. Individual cooling tower performance in 2012 was consistent with the performance recorded in 2011. Net cooling in the canal was 3.8°F, attributable to 0.2°F cooling in the canal and approximately 1.8°F for each tower. The net change from the intake to the end of the canal was 15.2°F. Unit 2 was refueled with the outage starting on September 9, 2012.

Figure 3-9 shows temperature measurements for 2013 when three cooling towers operated.

The average temperature rise through PBAPS was 18.9°F. Net cooling in the canal was S.0°F, attributable to 0.2°F cooling in the canal and approximately 1.6°F for each of the three towers.

The net change from the intake to the end of the canal was 13.9°F. Unit 3 was refueled beginning September 9, 2013.

2010: no towers in operation 110 105 100 95

~

!.. 90

~

~. 85 a.

E 80

~

75 I 70 65 60 0 6/15 6/25 7/5 7/15 7/23 8/4 8/14 8/24 9/3 9/13 Figure 3-6. Cooling water station data, 2010.

24

Final Report PBAPS Thermal Study 2011: one tower in operation 110 50 105 45 100 40

~

95 35

~

...3..

!.. 90 30 il

,.e! ii i! 85 25 0 if E 80 20 ii,.

~

75 15

~

II 70 10 65 5 60 0 6/15 6/25 7/5 7/15 7/25 8/4 8/14 8/24 9/3 9/13 Figure 3-7. Cooling water station data, 2011.

2012: two towers in operation 110 50 105 45 100 40 95 35 ~

~

....3 2- 90 30 i1 e!,. ~I i!

.... 85 25

~

E 80 20 fI

,;~~-- -- ---~~

15

~I 70 ~, i::nd of,canal_mi!JUS !nta~" iV"Jlll 10 65 5 60 0 6/15 6/25 7/5 7/15 7/25 8/4 S/14 8/24 9/3 9/13 Figure 3-8. Cooling water station data, 2012.

25

Final Report PBAPS Thermal Study 2013: three towers in operation 110 50 105 45 100 40

~

35

,,3,.

u:-

~ 90 30 il

~

r i!

.c

!r

.a.. 85 25

~

E 80 20 ~

~ n 15 31 70 10 65

~ 0 w ~ m ~ w ~ ~ ~ m ~

Figure 3-9. Cooling water station data, 2013.

The preceding graphical summaries of temperatures through the cooling water system show all data available for the June 15 to September 15 period. The analysis that follows here and in the next section examines the incremental cooling in Conowingo Pond due to the operation of an additional cooling tower both within the discharge canal and downstream in Conowingo Pond.

This analysis uses data that begins July 1 rather than June 15 because, as noted earlier, the 201 O data begins later in the summer and although each year is different with respect to flows, temperatures and meteorological conditions, using consistent dates provides some commonality of conditions.

The temperature reductions in the discharge canal are summarized in Table 3-3 for the common data period (July 1 to September 15). The table shows that canal temperatures decrease as each tower is added. The incremental change in temperature can be calculated by taking the differences in temperature reduction and by recognizing the 0.2°F cooling that occurs in the canal. The table shows that temperature reductions at the end of the canal average 1.6°F when each additional cooling tower is operated.

26

Final Report PBAPS Thermal Study Table 3-3. Summary of temperatures and temperature reductions in the discharge canal; averages for June 15 to September 15 data, when available.

2010 2011 2012 2013 No towers One tower Two towers Three towers Head of Canal (°F) 100.4 98.8 101 .1 98.0 End of Canal (°F) 100.2 96.8 97.2 93.0 Overall temperature reduction (°F) 0.2 2.0 3.9 5.0 Temperature reduction due to cooling 0.0 1.8 3.7 4.8 tower(s) (°F)

First Tower Second Tower Third Tower Average temperature reduction per 0.0 1.8 1.9 1.6 cooling tower (°F) 3.4 Effectiveness of Cooling Towers in Reducing Downstream Temperatures The analysis of cooling tower operations can be extended to a set of stations downstream of the discharge structure where thermal effects on aquatic resources, if any, could occur. An overview of the behavior of the thermal plume is helpful in understanding the results of this analysis.

The discharge structure releases heated water at 5 to 8 feet per second through fixed subsurface openings (Figure 2-3). The cooling water that emerges from the discharge structure is warmer than the adjacent waters of Conowingo Pond and therefore tends to rise to the surface. The cooling water is also moving substantially faster than the adjacent waters. Higher relative velocity promotes mixing with cooler water while buoyancy tends to restrict mixing.

Mixing occurs when parcels of adjacent, cooler water are entrained into the plume. Entrainment is greatest when plume and ambient velocities are most different. However, the entrainment process reduces the temperature of the plume and its velocity to the point that entrainment ceases when the plume is no longer moving faster than adjacent waters.

Entrainment cannot occur along the western edge of the plume inasmuch as the supply of cool, ambient water is limited by the plume's close proximity to the shoreline. The presence of the shoreline also explains another feature of the PBAPS thermal plume; high Susquehanna River flows tend to bend the plume along the shoreline and reduce mixing because of a reduced velocity difference.

The point at which entrainment ceases is the end of the near-field region. The near-field plume can be distinguished in the field by pronounced velocity and temperature differences. In fact, the near-field is defined as the region where plume dimensions are controlled by the velocity induced by the discharge structure. The surface area of the near-field region is relatively small and although some heat is transferred to the atmosphere in this region, the majority of the heat transfer takes place over large distances in the far-field region.

In the far-field region, the plume is no longer clearly recognizable by a core of elevated temperature and high velocity. Its trajectory is controlled by ambient velocities rather than the velocities induced by the design of the discharge structure. Turbulent mixing has ceased and the mixing that does occur is due to processes common to unheated waterbodies: wind and 27

Final Report PBAPS Thermal Study wave action, daytime heating and nighttime cooling as well as high flow events such as floods.

However, most of the heat added by PBAPS is transferred to the atmosphere in the far-field where small temperature increases above equilibrium temperature act over very large areas.

The following analysis will show the amount of cooling directly attributable to the operation of the cooling towers. Cooling is readily measured at stations in the near-field. Far-field temperatures are also reduced by the operation of the cooling towers; however, these are more apparent when modeled than observed, as will be shown in Section 7.1.

The downstream reductions in temperature relative to the Head of the Canal Station are shown in Table 3-4. These reductions in temperature are the result of a combination (1) heat transfer to the atmosphere in the canal and cooling towers; (2) entrainment of ambient water into the thermal plume in the near-field; and, (3) heat transfer to the atmosphere over large areas in the far-field. In gener~I. ~II ~tations ~how reductions in temperature as the number of operating cooling towers increases.

The relationship between incremental temperature reductions (Table 3-5) and the number of towers operating is not entirely linear and becomes less so farther downstream from the discharge canal. For example, at Station 215, the data indicate that the addition of a single tower can decrease temperatures by 1.3°F, 0.3°F, or 0.9°F. Farther downstream (e.g., Stations 189 and 401) the increment was negative, meaning an increase in temperature when another tower was added. The variations in temperature reductions are a consequence of changing Susquehanna River flows - high flows tend to push the thermal plume towards the western shoreline while promoting mixing with ambient water. The variations in temperature reductions are also a function of day-to-day weather which affects both cooling tower performance and cooling at the water surface.

The downstream stations shown in Table 3-4 and Table 3-5 can be more systematically studied by separating them into shoreline, nearshore and cross-river transects as shown in Figure 3-10.

Table 3-6 shows cooling tower effectiveness along the shallow shoreline stations downstream of the discharge canal. This table shows that there are clear temperature reductions down to and some distance beyond Station 215. Downstream of Station 215, there are temperature increases when additional towers operate. Increases are likely due to variations in conditions from the 2010 base year, especially the fact that Stations 189 and 190 are not always in the plume. Station 190 is located around a bend in Conowingo Pond, and away from the downstream-directed plume trajectory.

For the nearshore stations which measure deeper, offshore water that aligns more with the plume (Table 3-7), there is definite temperature reduction with the addition of towers to Station 301. However, the reductions are a surface phenomenon, as shown in Table 3-8, which shows both reductions and increases in the lower part of the water column. The cross-river transect only shows consistent temperature reductions to Station 301 (Table 3-9).

28

Final Report PBAPS Thermal Study Table 3-4. Downstream surface temperature reductions from the Head of Canal (°F); averages for June 15 to September 15 data, when available.

Temperature Reduction (°F)

Distance No towers One tower Two towers Three towers Primary temperature Station (miles) 2010 2011 2012 2013 reduction process Head of Canal 0.0 0.0 0.0 0.0 0.0 Cooling towers (when End of Canal 0.9 0.2 2.0 3.9 5.0 operating) 214 1.2 6.7 8.3 8.8 10.0 Entrainment 201 1.3 11 .7 12.4 13.9 14.6 215 1.5 8.4 9.7 10.0 10.9 301 2.1 9.6 9.8 11.9 12.5 Heat transfer to the 189 2.2 13.0 13.1 13.0 13.9 atmosphere 401 2.9 13.8 14.5 15.4 15.2 611 7.8 13.8 13.8 15.0 15.3 Table 3-5. Incremental surface temperature reductions as towers are added (°F); averages for June 15 to September 15 data, when available.

Distance Incremental Temperature Reduction (°F)

(miles) First Tower Second Tower Third Tower Head of Canal 0.0 - - -

End of Canal 0.9 1.8 1.9 1.2 214 1.2 1.6 0.5 1.2 201 1.3 0.7 1.5 0.7 215 1.5 1.3 0.3 0.9 301 2.1 0.2 2.1 0.6 189 2.2 0.2 -0.2 1.0 401 2.9 0.7 0.9 -0.2 611 7.8 0.0 1.2 0.4 29

Final Report PBAPS Thermal Study ea.ch Bottom Petera Creek

.tomlc: Power Station ,\ I* ti. ** - r ""

Endo'

,A Canal

zca l

Cross-river Bottom Beach Shoreline

/ .*

l" t '~q,l'-\~I.\

" -A. FraiWI' Tunnel

\I \II\ I ,"II I#'

!I

~

J 1

/

z' l

I .-,; I i'.;o.sta,& ith, ow..ctflN l'JAV'TEQ, Tbr'tTa ll ri'l'fl'lt J

WC- .

GMOt:.t K;N, ii9dntr1 t~L °""n.t'V.4 .Su'"'°"'- E.\11 l<o~: ono he GIS V.e1 ColT1U'*l'r 613

/

( Conowingo

!' Dam

r. '

Figure 3-10. Transects and stations used in the cooling tower analysis.

30

Final Report PBAPS Thermal Study Table 3-6. Incremental temperature reductions at shoreline stations; averages for June 15 to September 15 data, when available.

Incremental Temperature Reduction (°F)

Station Distance First Tower Second Tower Third Tower All Towers (mi)

End of Canal 0.00 1.8 1.9 1.2 4.9 214 0.37 1.6 0.5 1.2 3.3 215 0.65 1.3 0.3 0.9 2.5 189 1.32 0.2 -0.2 1.0 1.0 190 2.05 0.2 -1.0 1.2 0.4 Table 3-7. Incremental temperature reductions at nearshore stations - surface; averages for June 15 to September 15 data, when available.

Incremental Temperature Reduction (°F)

Station Distance First Tower Second Tower Third Tower All Towers (mi)

End of Canal 0.00 1.8 1.9 1.2 4.9 201 0.39 0.7 1.5 0.7 2.9 301 1.22 0.2 2.1 0.6 2.9 401 2.05 0.7 0.9 -0.2 1.4 611 6.95 0.0 1.2 0.4 1.6 Table 3-8. Incremental temperature reductions at nearshore stations - bottom; averages for June 15 to September 15 data, when available.

Incremental Temperature Reduction (°F)

Station Distance First Tower Second Tower Third Tower All Towers (mi)

End of Canal 0.00 1.8 1.9 1.2 4.9 201 0.39 -0.3 1.0 0.0 0.8 301 1.22 -0.3 1.1 0.1 0.9 401 2.05 -1.3 1.0 0.9 0.5 611 6.95 -1.5 2.5 1.1 2.1 31

Final Report PBAPS Thermal Study Table 3-9. Incremental temperature reductions at cross-river stations - surface ; averages for June 15 to September 15 data, when available.

Incremental Temperature Reduction ("F)

Station Distance First Tower Second Tower Third Tower All Towers (mi)

End of Canal 0.00 1.8 1.9 1.2 4.9 301 1.22 0.2 2.1 0.6 2.9 302 1.31 1.3 0.9 1.6 3.8 303 1.42 -0.2 0.8 1.5 2.1 304 1.56 1.8 0.7 1.4 3.9

3. 5 Conclusions Each of the four objectives of the temperature monitoring program was met:
  • Temperatures were recorded at the biological sampling stations and subsequently used to interpret biological data;
  • Temperatures throughout the Pond were measured over a representative range of Susquehanna River flows and temperatures, including periods of very low flows and high temperatures;
  • Temperature data were obtained for typical operations at Holtwood, Muddy Run, PBAPS, and Conowingo operations; and
  • Temperature data were used for hydrothermal model calibration and validation.

Analysis of the temperature data showed that:

  • The towers performed as designed; each tower cooled the discharge by about an additional 1.6°F, measured from the head to the end of the discharge canal;
  • Operation of the towers reduced water temperatures in Conowingo Pond by consistent and measurable amounts within 1.2 miles of the discharge and near the western shoreline and by smaller amounts beyond 1.2 miles where reductions were variable and related to ambient temperatures and Susquehanna River flows.

32

Final Report PBAPS Thermal Study 4 Representative Important Species (RIS)

Eleven fish species are designated as RIS for this demonstration as agreed upon with PADEP and in accordance with the study plan (Normandeau Associates et al. 2010). Nine of the species were evaluated as RIS in previous thermal effects demonstrations for PBAPS and were retained for this demonstration as agreed upon with PADEP. Most continue to be appropriate representative species for assessment of potential thermal impact consistent with the concept of RIS, as established by the USEPA (1977), e.g., recreational value, representative of the balanced indigenous community, or an important food item for other RIS. Two new fishes, Chesapeake Logperch and White Sucker, were added as RIS for this Demonstration at the request of PADEP. Although no federally-listed threatened or endangered species are present in Conowingo Pond, the Chesapeake Logperch was added because it was a candidate species in Pennsylvania at the start of the study. Subsequently, in December 2012, it was listed as threatened by Pennsylvania. The White Sucker is included because it is more thermally sensitive than many of the other RIS. No migratory fish are included as RIS. The eleven RIS are:

  • Bluegill (Lepomis macrochirus)
  • Bluntnose Minnow (Pimephales notatus)
  • Channel Catfish (lctalurus punctatus)
  • Gizzard Shad (Dorosoma cepedianum)
  • Largemouth Bass (Micropterus salmoides)
  • Logperch (Percina caprodes) renamed Chesapeake Logperch (P. bimaculata)
  • Smallmouth Bass (Micropterus dolomieu)
  • Spotfin Shiner (Cyprinella spiloptera)
  • Walleye (Sander vitreus)
  • White Crappie (Pomoxis annularis)
  • White Sucker (Catostomus commersonit)

This section provides basic life history and habitat preference information for each of the RIS.

4. 1 Bluegill Bluegill is a numerically abundant, recreationally important panfish that is widely distributed in shallow and deep habitats in Conowingo Pond. The species is prey for top carnivore species such as Largemouth Bass, Smallmouth Bass, Flathead Catfish, and Walleye.

Bluegill is most abundant along shoreline areas in lentic and lentic type environments such as ponds, lakes, reservoirs, and large, low velocity streams (Whitmore et al. 1960). In riverine habitats, Bluegill is mostly restricted to areas of low velocity (Hubbs and Lagler 1958). Adults prefer current velocities <0.3 ft/sec, but will tolerate up to 1.5 ft/sec (Hardin and Bovee 1978). In riverine environments, nest sites are selected for low flow velocity. Optimal lacustrine habitat is characterized by fertile lakes, ponds, and reservoirs with extensive littoral areas (Emig 1966; Scott and Crossman 1973). However, deeper areas are also required for overwintering and retreat from the summer heat (Scott and Crossman 1973). Cover in both lacustrine and riverine habitats in the form of submerged vegetation or logs and brush is utilized by the species, especially juveniles and small adults (Moyle and Nichols 1973; Scott and Crossman 1973).

33

Final Report PBAPS Thermal Study Nests are usually found in quiet, shallow 3.3-9.8 ft water (Swingle and Smith 1943). Although spawning can occur over almost any substrate, fine gravel or sand is preferred (Stevenson et al.

1969; Pflieger 1975).

4.2 Bluntnose Minnow Bluntnose Minnow is a numerically important prey species and together with Comely Shiner (Notropis amoenus), Spottail Shiner (Notropis hudsonius) and Spotfin Shiner represents an important forage base for the larger carnivorous fishes. The Bluntnose Minnow occupies a broad range of habitats including lakes, ponds, rivers, and streams. They prefer shallow areas of clear water with sand and gravel bottoms, but they are also found over mud and silt and/or aquatic vegetation. The Bluntnose Minnow exhibits great habitat plasticity (Jenkins and Burkhead 1993).

The spawning of Bluntnose Minnow typically occurs between late May and September.

Spawning takes place in pool shallows beneath stones or debris. When natural cavities are lacking, sometimes the male burrows through the silt to create a space beneath an object. The eggs are usually deposited in the cavities in a single layer, rarely in clumps (Jenkins and Burkhead 1993). Females of this genus are fractional spawners, i.e., they discharge eggs more than once during a spawning period (Gale 1983). Males defend the nest.

4.3 Channel Catfish Channel Catfish is abundant and widely distributed in Conowingo Pond and is important to anglers. It is most numerous in bottom trawl samples but is also among the most numerous species taken by electrofishing.

Optimum riverine habitat for Channel Catfish is characterized by warm temperatures (Andrews et al. 1972) and a diversity of velocities, depths, and structural features that provide cover and food (Bailey and Harrison 1948). Optimum lacustrine habitat is characterized by large surface area, warm temperatures, high productivity, low to moderate turbidity, and abundant cover (Davis 1959; Pflieger 1975).

Fry, juvenile, and adult Channel Catfish concentrate in the warmest sections of rivers and reservoirs (Ziebell 1973; Stauffer et al. 1975; McCall 1977). They strongly seek cover. Debris, logs, cavities, boulders, and cut banks in lakes and in low velocity (0.5 ft/sec) areas of deep pools and backwaters of rivers will provide cover for Channel Catfish (Bailey and Harrison 1948). Cover consisting of boulders and debris in deep water is important as overwintering habitat (Miller 1966; Jester 1971; Cross and Collins 1975). Deep pools and littoral areas (> 16 ft deep) with > 40% suitable cover are assumed to be optimum.

Channel Catfish usually spawn in secluded semi-darkened nests adjacent to large rocks, log jams, in holes, and in other types of cavities (Harlan et al. 1987).

4.4 Gizzard Shad Gizzard Shad is the most abundant fish in Conowingo Pond and the young are important prey species. It was inadvertently introduced into (approximately 100 individuals) Conowingo Pond in 1972 (two years prior to PBAPS start-up) during American Shad trial transports. Hundreds of 34

Final Report PBAPS Thermal Study thousands of Gizzard Shad are transported into Conowingo Pond each spring via the East Fish Lift at Conowingo Dam. This species is often the most abundant species in trawl and electrofishing samples. It uses other upstream fishways as well and has become well established throughout the lower Susquehanna River.

The Gizzard Shad is common in lakes, oxbows, impoundments, sloughs and large rivers with low gradients (Etnier and Starnes 1993), but reaches greatest abundance in waters where fertility and productivity are high (Robison and Buchanan 1988). Gizzard Shad avoid high gradient streams and rivers in the mountains and rivers without large, permanent pools, but can tolerate moderately turbid and, occasionally, even brackish or salt waters (Trautman 1981; Robison and Buchanan 1988).

The Gizzard Shad prefers living in open water, at or near the surface (Becker 1983; Harlan et al.

1987). The young may select for areas of aquatic vegetation (Hubbs and Lagler 1943). If the oxygen supply is adequate, the species may descend to depths as great as 108 feet, as in Norris Reservoir, Tenn. (Dendy 1945). In the Coosa River, Alabama, Gizzard Shad were found in deep (greater than 25 feet) as well as shallow water (Scott 1951).

Typically found traveling in schools, juveniles are non-visual planktivores, most commonly utilizing zooplankton and phytoplankton in the diet. Adults are primarily bottom filter-feeding detritivores; eating large quantities of organisms attached to underwater surfaces, especially from littoral areas. Gizzard Shad also feed on phytoplankton in open water (Sublette et al.

1990).

Gizzard Shad spawn in spring and early summer, usually in shallow water when water temperatures reach 50°F to 70°F (Williamson and Nelson 1985). Spawning usually occurs at near surface depths (1.0 to 5.2 ft), but sometimes as deep as 49 ft, and sometimes over vegetation or debris (Jones et al. 1978, Miller 1960, Wang and Kernehan 1979). Spawning groups swim near the surface and roll about as a mass, ejecting eggs and sperm (Miller 1960).

Eggs are demersal and, after slowly sinking, adhere to algae, rocks, and other objects (Miller 1960). Young-of-the-year Gizzard Shad travel in compact schools soon after hatching, but by fall most of the schools disperse and few form the following spring, at least in Norris Reservoir; schooling largely ceases by the time the shad are a year old (Dendy 1946).

4.5 Largemouth Bass Largemouth Bass is greatly valued by anglers and is found more abundantly in the southern half of Conowingo Pond as compared to the Smallmouth Bass which is more numerous in the northern half. Lacustrine environments are the preferred habitat of Largemouth Bass (Emig 1966; Scott and Crossman 1973). Optimal riverine habitat for Largemouth Bass is characterized by large slow moving rivers or pools of streams with soft bottoms, some aquatic vegetation, and relatively clear water (Trautman 1981; Larimore and Smith 1963; Scott and Crossman 1973).

Deacon (1961) reported that Largemouth Bass abundance increased in rivers during dry years when the flow was reduced and the water pooled. Thus, it is assumed that a river with a high percent (- 60%) of pool and backwater area is optimal. Largemouth Bass has considerable 35

Final Report PBAPS Thermal Study tolerance to high water temperatures as demonstrated by its widespread distribution in the southern United States.

Much like Bluegill and Smallmouth Bass, males prepare a nest over clean hard substrates, spawn singly with one or more females in the nest, and then drive away all other fishes and other large invaders. A gravel substrate is preferred for spawning (Robinson 1961; Mraz 1964),

but Largemouth Bass will nest on a wide variety of other substrates, including vegetation, roots, sand, mud, and cobble (Harlan et al.1987; Mraz et al. 1961). Nests are constructed by the male at water depths averaging 1 to 3 ft, with depths ranging from about 0.5 to 25 ft (Allan and Romero 1975). The adhesive eggs in the nests are aerated by swimming motions of the male, and the eggs and young are guarded against predators.

4. 6 Chesapeake Logperch Chesapeake Logperch is a small to medium size fish (length up to 7 in) in the perch family. The Chesapeake Logperch was recently removed from taxonomic synonymy with the widely distributed Logperch (Percina caprodes) and recognized as a distinct and valid species with limited distribution restricted to the Chesapeake Bay watershed (Near 2008). Little is known about this species and its habitats, but it occurs primarily in larger waterways and lowermost sections of tributaries. Chesapeake Logperch occurs in the lower Susquehanna River primarily in tributaries to the Conowingo Pond and below Conowingo Dam and occurs sporadically in Conowingo Pond.

Logperch inhabit mud-bottomed, sandy, gravelly and rocky areas in big lakes. They can be found living over those bottom types in large rivers. They tend to stay offshore in water deeper than three or four feet, and have been captured at depths of more than 130 feet in Lake Erie.

Logperch tolerate a wide variety of habitats. During its spawning runs, the Logperch swims from the larger waterway in which it makes its usual home into smaller tributary streams, where for a short time the fish is abundant (Etnier and Starnes 1993).

Logperch relate intimately to bottom substrate. At night Logperch seek cover and become quiescent (Emery 1973). Trautman (1981) reported that during sunny days they hide under rocks or bury in sand with only the eyes exposed. Logperch feed benthically and may overturn stones by using their snouts to uncover food items (Jenkins and Burkhead 1993).

4. 7 Smallmouth Bass Smallmouth Bass is highly valued by anglers but, like other game fishes that are present in the fish community in Conowingo Pond, it occurs in relatively low numbers. While commonly considered a cool water species, Smallmouth Bass has considerable tolerance to high water temperatures, as demonstrated by its widespread distribution in the southern United States and tolerance to high water temperatures as reported by Wrenn (1980), Mathur et al. (1983) and others.

Smallmouth Bass prefer large, clear lakes and clean streams with abundant cover. It is an important sport fish in the Susquehanna River, particularly in the riverine reaches and larger tributaries. Smallmouth Bass is usually more numerous in the upstream reaches of reservoirs, as is the case in Conowingo Pond.

36

Final Report PBAPS Thermal Study Smallmouth Bass spawn on rocky lake shoals, river shallows, or backwaters or move into creeks or tributaries to spawn (Harlan et al. 1987, Coble 1975, Clancey 1980). Smallmouth Bass spawned in warm sloughs or backwater areas bordering the Columbia River (Montgomery et al. 1980). The species requires a clean stone, rock, or gravel substrate for spawning (Robbins and MacCrimmon 1974). Studies show that the habitat condition during spawning is the most important factor for year class strength in Smallmouth Bass (Clancey 1980).

Smallmouth Bass exhibits strong, cover-seeking behavior and prefer protection from light in all life stages (Coble 1975; Miller 1975). Deep, dark quiet water is used for cover (Coble 1975), but bass use all forms of submerged cover, such as boulders, rocks, stumps, root-masses, trees, and crevices, without apparent preference for any one type (Hubert and Lackey 1980).

In lakes and reservoirs, adults most often use cooler areas, such as drop-offs, that are away from vegetation and in water <39 ft deep (Scott and Crossman 1973; Coble 1975). In a Tennessee River reservoir, adults were frequently in water >33 ft deep during the summer (Hubert and Lackey 1980).

Nests are usually constructed in water from 1 to 3 ft deep (Coble 1975), but may be built in water up to 23 ft deep (Mraz 1964; Robbins and MacCrimmon 1974). Nests are commonly in gravel or broken rock (Latta 1963; Mraz 1964); near boulders, logs, or other cover (Scott and Crossman 1973); in shallows or backwaters of streams (Clancey 1980); or in protected bays or shoals in lakes (Robbins and MacCrimmon 1974). Nests are also made over bedrock, rootlets in silt, or sand, but these substrates are less commonly used (Cleary 1956; Latta 1963; Scott and Crossman 1973). Nests are usually in areas of quiet water (Pflieger 1975) or very slow current (Robbins and MacCrimmon 1974).

4. 8 Spotfin Shiner Spotfin Shiner, a small-bodied minnow like the Bluntnose Minnow and Comely Shiner, is a numerically important member of the fish community throughout Conowingo Pond and serves as an important prey item for top carnivore fishes. It is a warm water species and is most characteristic of medium to large streams and rivers (Jenkins and Burkhead 1993). It is found over mud, sand and gravel (Becker 1983). In Conowingo Pond, Spotfin Shiner was found mostly in shallow nearshore habitats sampled by seine and electrofishing and not in the more open-water and bottom habitats sampled by bottom trawl.

The Spotfin Shiner is an active mid-depth feeder on drift and to a lesser degree on bottom organisms (Jenkins and Burkhead 1993).

Spotfin Shiner is a scatter spawner and typically spawns in shallow runs or riffles, either on unmodified gravel substrate or over minnow nests, sucker redds, or nests of other species or on the underside of submerged logs and roots (Pflieger 1975, R. J. Miller 1964). Spawning sites are chosen over irregular surfaces so the eggs can be deposited into small crevices where they are safe through incubation.

37

Final Report PBAPS Thermal Study 4.9 Walleye Walleye is of interest to anglers in Conowingo Pond but, like Smallmouth Bass and Largemouth Bass, has never been numerically important in the sampling programs for PBAPS. Walleye tolerate a wide variety of environmental conditions but are reported to be most abundant in large-to-medium lakes and riverine systems characterized by cool temperatures, shallow to moderate depths, moderate turbidities, extensive littoral areas, extensive areas of clean rocky substrate, and mesotrophic conditions (McMahon and Nelson 1984).

Adult Walleye generally are found under cover in moderately shallow (< 50 ft) waters during the day and move inshore at night to feed (Johnson and Hale 1977; Ryder 1977). Adults often are found in areas with slight currents (Ryder 1977), except during the winter when they tend to avoid turbulent areas (Colby et al. 1979).

Habitat requirements for juvenile Walleye seem to be similar to those of adults (Colby et al.

1979). The critical velocity for juveniles with a fork length of 7.9 in is 2 ft/sec (Jones et al. 1974).

Preferred spawning habitats are shallow shoreline areas, shoals, riffles, and dam faces with rocky substrate and good water circulation from wave action or currents (Johnson 1961; Colby et al. 1979).

4.10 White Crappie White Crappie had historically been an abundant and recreationally important panfish in Conowingo Pond but, following introduction in the 1970's of Gizzard Shad with which it competes for planktonic food when young, is no longer numerically important in the fish community. It occupies both pelagic and shoreline habitats. White Crappie can be abundant as pelagic schools in turbid reservoirs. Spawning occurred in shallow water (< 1O ft) in association with submerged aquatic vegetation and gravel/stone substrates (Cooper 1983). White Crappie are most numerous in base-level, low gradient rivers (Trautman 1981; Smith and Powell 1971).

4. 11 White Sucker The monitoring data show that White Sucker is not numerically important in Conowingo Pond, but it is one of the most thermally sensitive species in the fish community. White Sucker is more numerous in small rivers and streams rather than major rivers and is also found in warm and shallow lakes and tributary rivers of larger lakes. In many North American lakes and reservoirs, each year in early spring large numbers of White Sucker migrate up tributary streams to spawn.

White Sucker also is very tolerant of pollution, turbidity, and low oxygen levels.

White Sucker feeds primarily upon the bottom (except for a short period of life during which they feed upon plankton near the surface), consuming midge larvae and small crustaceans, aquatic insects and other arthropods, snails, clams, fish eggs, and detritus (Jenkins and Burkhead 1993).

Stream populations of White Sucker reach maximum abundance in low to moderate gradie~t streams (Stewart 1926). Larger White Sucker (>6 in TL) primarily inhabit pools (Propst 1982) and are common in areas of slow to moderate velocity (approximately 1.3 ft/sec), although 38

Final Report PBAPS Thermal Study smaller individuals (<6 in TL) occur in a greater variety of habitats than adults (Scherer 1965, Pflieger 1975, Propst 1982).

39

Final Report PBAPS Thermal Study 5 Biological Monitoring and Assessment

5. 1 Introduction This section describes the benthic macroinvertebrate and fisheries components of the thermal effects study as well as the temperature monitoring at the biological stations. As described in the Study Plan, the primary objectives of the biological monitoring component of the study are to:
  • Document the spatial and temporal distribution of fishes within the thermal plume and relative to areas of the Pond outside of the thermal plume;
  • Document the relative abundance of fishes within the thermal plume and relative to areas of the Pond outside of the thermal plume;
  • Determine the relative condition of fishes within the thermal plume and relative to areas of the Pond outside of the thermal plume;
  • Document the spatial and temporal distribution of benthic macroinvertebrates within the thermal plume and relative to areas of the Pond outside of the thermal plume; and
  • Document the relative abundance of benthic macroinvertebrates within the thermal plume and relative to areas of the Pond outside of the thermal plume.

Sampling for the first year of the monitoring program, 2010, was performed in July through October. During 2011 - 2013 biological collections were completed monthly from April through October, with additional boat electrofishing sampling completed during winter (January-March) 2011, 2012, and 2013. Temperature monitoring at the biological monitoring stations was restricted to July to October 2010 and April to October for 2011 through 2013.

Overall, during the 4 years of the study a total of 224 benthic macroinvertebrate samples were collected at a total of 10 stations (Figure 5-22). For fish, extensive collections were completed to determine their distribution and relative abundance within and outside of the thermal plume. A total of 673 collections were completed using trawl, seine, and boat electrofisher at 30 stations (Figure 5-22 through Figure 5-24). Figure 5-25 provides the location of both benthic macroinvertebrate and fish collection stations.

Methodologies and analyses for the temperature monitoring, benthic macroinvertebrate community sampling, and fish community surveys are summarized below.

5.2 Biological Station Temperatures The temperature record observed at the biological stations is critical to understanding the influence of the PBAPS thermal plume on the biological community. Continuous temperature monitoring was completed at all of the benthic macroinvertebrate, electrofishing, and seining collection stations. Monitoring was performed in situ using Onset HOBO Pro v2 Water Temperature Data Loggers. These instruments are accurate to 0.36°F in the range 32°F to 122°F, can resolve temperatures to 0.04°F at 77°F, and have a five-minute response time in water. The loggers recorded water temperature every 15 minutes and were located in shallow shoreline locations (<5 ft water depth) on the river bottom where complete mixing of the water column occurs (see Section 3 for monitoring detail).

40

Final Report PBAPS Thermal Study For the purposes of this analysis, a subset of the monitoring stations not influenced by the thermal plume (208, 220, PBAPS Intake) and all thermally influenced stations (214, 215, 189, 190, 216, and 217) will be characterized. The PBAPS Intake monitor was installed specifically for this study and is at a different location than the station's water temperature monitor used for operational purposes. Note that although Station 208 is located along the east shoreline of the Pond and upstream from the end of the discharge canal it does experience an increase in water temperature resulting from the PBAPS thermal discharge at low river flows during the summer months. This phenomena is coincident with River flows less than 12,000 cfs and MRPSF pumpback operations (Normandeau and Gomez and Sullivan Engineers 2012). Additionally, Station 208 is located along Peach Bottom Beach, a shallow portion of the Pond which experiences solar heating and limited water flow during lower flow conditions. Thermally affected electrofishing Station 161 is characterized by the monitoring at Station 214 (a seine and benthos station) Thus, a separate water temperature monitor was not installed at Station 161.

Water temperatures measured in Conowingo Pond over the course of the study period (April 1 to October 31) followed a typical seasonal pattern for the Susquehanna River with warmest temperatures observed during July and August. Figure 5-1 through Figure 5-18 provide daily mean and daily instantaneous maximum water temperatures for each monitoring location during each year of the study. The highest water temperatures at the biological monitoring stations were observed in July and August at Station 214, which is along the west shoreline and is the monitoring location closest to the end of the PBAPS discharge canal. Water temperatures decreased in a downstream direction at monitoring locations farther downstream from the end of the discharge canal. The lowest ambient water temperatures were observed at Station 220, which is upstream from the PBAPS intake along the west shoreline.

Inter-annual variation in water temperature was also evident with 2010 generally warmer than 2012 and 2012 generally warmer than 2011. Water temperatures in 2013 were generally cooler than the 2010, 2011, or 2012 with ambient water temperatures exceeding a daily mean of 80°F for only a short portion of June and August, and a few weeks in July (Figure 5-1 and Figure 5-2).

The greatest contrast in ambient water temperatures among years occurred during mid-July through August 2013 when temperatures have typically been the highest. In 2013 ambient water temperatures were 6-8°F lower from mid-July through August compared to the same time period during the previous three years (Figure 5-1 and Figure 5-2). A similar pattern of lower water temperatures during mid-July through August in 2013 was also observed at the thermally influenced locations (Figure 5-4 through Figure 5-9). Water temperature was generally cooler in 2013 with fewer days of temperature exceeding 90°F as daily or instantaneous maximum at the thermal stations (Table 5-1 through Table 5-4). However, the number of days that exceeded 80°F as instantaneous maximum at the thermal stations was higher in 2013. This resulted from ambient water temperatures being warmer in May and October 2013 compared to the previous years.

Weekly swings in water temperature resulting from variation in ambient temperature were also evident. For example, Station 215 water temperatures were warmer in 2012 from the end of June through mid-July and then warmer during 2011 for the remainder of July (Figure 5-5). This 41

Final Report PBAPS Thermal Study pattern of inter-annual variation was evident at both the upstream and downstream stations and is related to the complex interaction of ambient water temperatures and River flows.

Table 5-1 through Table 5-4 provide a summary of the of the instantaneous maximum and mean daily water temperatures for the monitoring locations during each year of the study. Each table provides a count of the number of days that instantaneous and daily mean water temperature exceeded 80 and 90°F for each station. The basis for these two water temperature values was that 80°F corresponds to a normal summer condition (discussed further in Section 7) and 90°F corresponds to a temperature that does not typically occur under natural conditions in the Pond. The purpose was to provide a comparison of these two temperature points among the monitoring stations.

In 2013, water temperatures were cooler than the previous years, with a fewer number of days that ambient water temperatures exceeded 80°F as instantaneous maximum or daily mean.

Similarly, the thermally influenced stations in 2013 had a fewer number of days exceeding 90°F as instantaneous or daily mean compared to previous years. Overall, the monitoring data indicate that the warmest water temperatures were observed during 2012 for all locations.

However, the water temperatures observed in 2010 were also high but the monitoring period was abbreviated (not initiated until July 28) and not directly compareable to other years in terms of absolute number of days exceeding 80 or 90°F.

As noted above, the highest water temperatures were observed to occur in July and August.

Therefore, analyses of potential thermal effects on benthic macroinvertebrates and fish will focus on these months. However, the cumulative effects of elevated temperatures during the course of the year will also be considered. These types of cumulative effects, as opposed to just the highest temperatures in July and August, may potentially alter the aquatic assemblage, in particular, at the near-field stations (Stations 161, 214 and 215). Cumulative effects of elevated water temperatures will be evaluated for fish by documenting body condition, disease occurrence, length/age structure, and retrospective analysis of relative abundance. In addition, cumulative effects will be elucidated in comparisons of fish and benthic macroinvertebrate community composition (e.g. species richness, diversity and evenness) between thermally influenced and non-thermally influenced collection locations.

42

Final Report PBAPS Thermal Study IW

-1010 StationZZO -1mt

- - 2012

-ZOil 80

  • o 4/1 4/JJ 4(15 'i/7 'j/ 19 5/31 6/ll 6/24 7/6 7/UJ 7/'JO Y/11 8/23 'J/4 9/16 9/28 tQ/10 lU/21 Figure 5-1. Daily mean water temperature measured at Station 220, 2010-2013.

Data not recovered for portions of August and September.

.... PBAPS Intake - 1010

-2ou 2012

-1011

... 4/1 4/lJ ~/l"' r,/ I ~/1'J ~/j 1 riltl tj(bt l /h /I ll! I f., NIU tUJJ Q/4 9/ 111 qJ/H. HJ(lU 10/21 Figure 5-2. Daily mean water temperature measured at PBAPS Intake, 2010-2013.

43

Final Report PBAPS Thermal Study

!ID Station 208 -1010

-2011

- JOU 40

-A/l .J/13 .S/2'";, .,17 5/J9 5/3\ f!/1Z 6/J.4 7/6 7/J8 7/'YJ 8/Jt RfJJ 9/1. ':l/Ui 9/111 W/JO W/11 l

  • Figure 5-3. Daily mean water temperature measured at Station 208, 2010-2013.

tal

-)1)10 Station 214 -2011 lOU

- 101!

90 811 411 4/1 4/1\ A/ /\ ".J/I ~ / 11J ';/U b/11 b/J" l/b 1/t8 l/JJ 6/11 tenJ fJ/4 9/11'.J '4//fl. l i.V1iJ tO/ll Figure 5-4. Daily mean water temperature measured at Station 214, 2010-2013.

44

Final Report PBAPS Thermal Study 100

-.2010 Station215 -1011

- 10121

-2011 i! 10

.ii i

lli

'" */1 4/H 4/1!; 'JI'/ .,,I C) Vil h/1J b/14 1/1'1 OttJ ,, ,, f/11 S/IJ l.f/'4 !4/1h ~/Jd 10/JO JO/Jl Figure 5-5. Daily mean water temperature measured at Station 215, 2010-2013.

"" Station 189 -

1010

-l01\

"' ll/1 4i1l *t/l!'I ':J/I )./111J ">/ '1 b/ 11 b/14 I/It 1/t 8 l/.IJ ~ 1 11 H/2J 'J/ 4 q/1 1J Y/l.A 10/10 10/U Figure 5-6. Daily mean water temperature measured at Station 189, 2010-2013.

45

Final Report PBAPS Thermal Study lW Station 190 -1010

-2011

- 1011 40 4/1 4/lJ 4//!J ':Jfl !;/l~ ~/Jl bill b/l~ 11& 1/\8 l/!JJ K/11 'l'i/H 'J/11 1 1/16 'J/18 1~10 lU/1.1 Figure 5-7. Daily mean water temperature measured at Station 190, 2010-2013.

100 Station 216 -?.010

-1011

- 11111 Ill) 4/1 .s/13 I.fl') '/7 5/J9 ~/31 f./12 6/1A 1/6 7/18 7/30 8/Jl R/ Jl 'V'- 9/1L 9/21 tcVtO JCV12 Figure 5-8. Daily mean water temperature measured at Station 216, 2010-2013.

46

Final Report PBAPS Thermal Study 100 Station 217 -1010

-1011

- 1011 I

l 10

~

t:

40 i/I "1/13 4(1~ ~1/1 ':J/t~ '1/31 6/11 b/2C 116 1/1H 1/~J K/ 11 KfH *j/IJ 'J/16 'J/18 IC/\U 10/lJ Figure 5-9. Daily mean water temperature measured at Station 217, 2010-2013.

HD

-JIJtO Station220 -.1011

- l012

-ion llO t.

l

(! 70 I

I w 40 4(1 J./13 4/2S "/7 ';/JCJ ~/31 f./12 6/2A 7/6 7/18 7/30 8/Jl 8(1l 914 ~/lfi 9/28 lCVJO HV'll Figure 5-10. Daily maximum instantaneous water temperature measured at Station 220, 2010-2013.

47

Final Report PBAPS Thermal Study

"" PBAPS Intake

- l ' OID

-1011

- 2012 I!

... /()

j 6U 40 4/1 4/1J 4/15 '>fl 5/19 ~/.11 fJ/11. fJ/14 1/6 //Ht I/JO H/11 H/23 *J/4 fl/lb ')/la JU'lU \U/ll Figure 5-11. Daily maximum instantaneous water temperature measured at PBAPS Intake, 2010-2013.

Station 208 - ) 010 80 t

~ 70 JO *

~~ w w ~ ~~-~~~-~ w --~~

Figure 5-12. Daily maximum instantaneous water temperature measured at Station 208, 2010-2013.

48

Final Report PBAPS Thermal Study tftl

-1010 1 Station214

-10111

.!01.l

-JOtl E eo I

l i

70 I

I till 40 Figure 5-13. Daily maximum instantaneous water temperature measured at Station 214, 2010-2013.

1011

-1010 1 Station215 -10111

- 1011

-wu j 8tl ~

Figure 5-14. Daily maximum instantaneous water temperature measured at Station 215, 2010-2013.

49

Final Report PBAPS Thermal Study

"" Station 189 - 1010 i!

... 70 i2

  • o 4/ 1 4/U 4il':l 'l(I 'l/l'lf 't/:H bill b/I.~ 116 1/\tJ f/!AJ K)tJ f,/23 'J/4 IJ/16 'J/18 1U'10 \~l.J Figure 5-15. Daily maximum instantaneous water temperature measured at Station 189, 2010-2013.

l Station 190 90 I

HO 40 tlfl 4/B 4/l., VJ ')/19 \/U h/ll tiJl,1 1/6 I/ti! IH) 11/11 I/" 1 1/4 ~/lb 'l/lr4 10/IO Hl/Jl Figure 5-16. Daily maximum instantaneous water temperature measured at Station 190, 2010-2013.

50

Final Report PBAPS Thermal Study lW

- 2 01D Station 216

!JO 80 E

l

.. 70

~E i

ii

~~~~ - ~~-mo~--~---~

Figure 5-17. Daily maximum instantaneous water temperature measured at Station 216, 2010-2013.

HIJ

-1010 Station217 i

!* 70

~

I* 60 40 Figure 5-18. Daily maximum instantaneous water temperature measured at Station 217, 2010-2013.

51

Final Report PBAPS Thermal Study Table 5-1. Summary of instantaneous maximum and mean water temperature data for multiple locations within Conowingo Pond in 2010.

Number of Days Instantaneous Maximum Number of Days Mean Temperature Temperature Station >90°F >80°F >90°F >80°F 220 0 34 0 28 PBAPS Intake 0 38 0 29 208 14 so 2 38 214 46 65 44 64 215 43 65 34 62 189 18 51 10 42 190 10 43 5 35 216 * * *

  • 217 * * * *
  • stations not monitored in 201 O Table 5-2. Summary of instantaneous maximum and mean water temperature data for multiple locations within Conowingo Pond in 2011.

Number of Days Instantaneous Maximum Number of Days Mean Temperature Temperature Station >90°F >80°F >90°F >80°F 220 3 55 0 38 PBAPS Intake 1 60 0 41 208 17 75 10 56 214 74 105 70 104 215 70 104 45 102 189 32 96 21 82 190 22 82 14 72 216 20 87 15 72 ---

217 16 80 8 69 52

Final Report PBAPS Thermal Study Table 5-3. Summary of instantaneous maximum and mean water temperature data for multiple locations within Conowingo Pond in 2012.

Number of Days Instantaneous Maximum Number of Days Mean Temperature Temperature Station >90°F >80°F >90"F >80°F 220 0 76 0 55 PBAPS Intake 0 77 0 69 208 18 58 3 48 214 84 127 73 122 215 78 124 54 117 189 43 108 19. 97 190 30 99 8 84 216 30 99 7 85 217 14 96 1 84 No data recovered for Station 208 from 8/8/12 to 9/6/12 Table 5-4. Summary of instantaneous maximum and mean water temperature data for multiple locations within Conowingo Pond in 2013.

Number of Days Instantaneous Maximum Number of Days Mean Temperature Temperature Station >90"F >80°F >90°F >80°F 220 0 43 0 25 PBAPS Intake 0 45 0 29 208 7 82 0 57 214 40 133 20 117 215 28 124 13 106 189 8 106 5 89 190 216 5

6 93 93 0

0 71 71


___ ___,._ -~

217 3 82 1 63 53

Final Report PBAPS Thermal Study 5.3 Dissolved Oxygen Conditions Dissolved oxygen (DO) concentrations in the subsurface waters of Conowingo Pond are important in assessing the potential suitability of fish habitat that is thermally available outside of areas that are avoided because they contain water temperatures in excess of a specified avoidance temperature. As mentioned in Section 2.2, previous studies, such as Mathur et al.

(1988), have shown that low DO concentrations tend to occur in the summer when ambient water temperatures exceed 75°F and Susquehanna River flows are less than 12,000 cfs, particularly in deeper areas in the lower third of the Pond.

In the present study, DO levels were not investigated in detail but DO concentrations and water temperatures at the surface and bottom of the Pond were routinely collected during trawl sampling (Figure 5-24). These data are summarized for 2010 through 2012 in Table 5-5 through Table 5-7. As in the previous studies, the lowest DO values (<5 mg/I) tended to occur in the deeper areas of the Pond, along the McClelland's Rock and Broad Creek transects, in July and August concurrent with River flows generally <12,000 cfs. Surface DO concentrations were relatively high and generally similar among transects. High plume temperatures did not appear to be associated with low DO values.

A more extensive DO study was performed in 1999 as reported in Normandeau (2000).

Dissolved Oxygen profiling was conducted in July and August on a weekly basis at west, mid-Pond, and east locations on four transects over a wide range of conditions: Fishing Creek (in the upper third of the Pond), Burkins Run Oust below PBAPS), Williams Tunnel (between Burkins Run and the PA/MD state line), and State Line. Figure 5-19, taken from Normandeau (2000), shows the average weekly surface and bottom DO concentrations taken along the four transects, and shows that surface DO concentrations were generally similar among transects.

However, corresponding bottom DO values were lower in June through much of August, particularly at the deeper water stations along the east shore on Williams Tunnel and State Line transects, as shown in Table 5-8, also taken from Normandeau (2000).

54

Final Report PBAPS Thermal Study Table 5-5. Dissolved oxygen and water temperature measured during trawl collections in Conowingo Pond, July through October 2010.

12 & 13 July 2010 Flow: 7, 759& 12,192 cfs McClellan's Rock Below Burkins Run Below PBAPS Broad Crvek PBAPS lnta ke StaUon No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. (°F)

Surface Start 90.0 91.4 90.5 97.2 87.8 88.7 86.4 90.0 87.8 87.4 86.4 86.9 87.8 85.1 86.4 86.0 End 94.1 87.4 89.1 97.3 88.7 90.0 89.2 90.0 87.8 89.1 86.7 87.8 88.2 86.0 86.4 86.4 Bottom Start 84.2 88.7 83.8 86.0 84.6 82.8 88.7 84.2 84.6 87.4 87.4 86.4 84.2 82.8 84.6 86.0 End 88.2 82.4 82.0 93.2 85.1 83.3 88.9 84.7 83.5 86.0 86.7 88.7 88.2 82.4 82.0 84.4 Dia Oxygen (mg/I)

Surface Start 8.5 8.0 8.4 8.0 8.4 8.0 8.0 8.0 7.9 8.4 7.2 7.8 7.2 7.8 7.4 7.8 End 8.1 8.5 7.9 7.8 8.2 5.5 7.9 8.3 7.2 8.3 6.2 7.2 7.4 8.2 7.3 7.8 Bottom Start 7.2 7.8 6.8 7.5 7.5 7.8 7.2 6.8 7.8 8.5 6.5 7.0 3.5 7.1 7.2 7.6 End 6.2 6.7 6.7 7.8 6.8 6.8 7.6 7.1 7.0 8.7 5.4 5.8 4.9 7.2 6.3 6.7 16 & 17 Auaust 2010 Flow: 7,812 & 9,n7 cfs Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. (°F)

Sutface SIBrt 89.6 88.2 87.8 95.4 88.2 87.4 86.9 88.2 84.6 85.1 85.1 86.0 84.6 82.8 83.8 84.6 End 83.8 86.0 80.6 83.3 82.0 81 .0 85.1 81.0 81 .0 82.4 84.7 82.4 80.6 79.7 80.2 80.6 Bottom Start 90.0 87.3 87.4 91.8 85.8 86.0 85.8 85.8 84.4 85.5 85.1 88.0 86.9 81 .5 82.4 83.8 End 81 .0 81 .3 80.2 61 .7 82.4 80.2 84.7 83.7 82.4 81 .1 84.9 81.9 84.0 79.5 80.2 81 .0 Dia Oxygen (mg/I)

Surface Start 7.5 7.5 7.8 7.5 8.2 7.4 7.8 7.5 8.0 7.6 7.2 7.5 7.0 7.9 7.9 7.5 End 6.2 5.8 6.6 6.8 6.5 6.0 7.3 6.8 7.0 8.1 7.0 4.8 4.3 6.7 7.0 6.9 Bottom Start 7.7 7.8 7.9 7.6 8.0 7.5 7.3 7.8 7.6 7.3 7.1 7.6 7.2 7.5 8.0 7.8 End 6.0 6.6 6.8 5.9 6.6 5.9 6.4 7.4 7.1 8.2 6.6 5.4 6.0 6.2 7.0 7.2 20 & 21 September 2010 Flow: 4,966 & 4,501 cfs Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. (°F)

Surface Start 80.2 76.1 76.1 81.0 76.1 76.6 75.2 74.3 75.6 75.2 74.3 75.6 76.1 75.2 75.2 73.8 End 82.4 79.0 75.7 82.8 76.1 76.6 n.2 82.6 76.1 76.1 75.2 76. 1 76.1 73.9 74.8 73.6 Bottom Start 75.9 75.2 74.8 n .o 76.1 75.2 n .o 75.2 75.6 75.2 75.2 75.2 75.2 75.6 73.8 72.0 End 73.0 76.6 73.9 n.5 76.1 75.2 n.o 80.4 76.1 76.1 75.4 75.4 75.6 73.9 74.7 72.7 Dlaa. Oxygen (mg/I)

Surface Start 6.4 8.2 6.6 8.8 8.8 8.0 9.0 9.0 8.4 6.8 7.2 7.6 8.2 9.2 9.2 7.9 End 8.8 8.4 8.8 9.2 8.9 8.4 8.5 9.1 8.6 8.0 7.6 8.0 8.0 9.5 9.3 8.5 Bottom Siert 8.0 7.6 6.5 7.5 8.6 6.2 8.8 8.4 8.4 6.5 6.9 7.8 7.5 9.4 7.8 6.7 End 8.0 7.6 7.5 8.5 8.6 6.2 8.4 9.3 8.5 7.9 7.3 7.2 7.3 9.5 8.9 7.2 18 & 22 October 2010 Flow: 23 586 & 23 024 cfs Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ('F)

Sutface Start 63.0 57.0 56.8 69.8 58.8 59.4 61 .7 62.2 58.1 58.6 60.4 59.7 57.6 57.6 57.6 58.1 End 66.4 55.8 55.8 58.6 58.1 57.4 58.8 57.6 57.9 57.9 59.9 58.6 55.8 57.0 57.6 56.1 Bottom Start 57.4 57.0 55.9 70.0 57.9 59.4 59.0 69.4 57.0 57.2 59.5 58.6 57.0 57.6 57.6 58.1 End 56.8 55.8 55.8 68.9 57.4 57.2 58.5 68.4 57.0 57.4 59.4 58.5 55.8 57.2 57.6 57.9 Dia Oxygen (mg/I)

Surface Start 11 .2 11.5 11.1 10.2 10.5 10.6 10.3 10.8 10.8 10.3 10.6 10.7 10.8 10.8 10.5 10.6 End 10.8 10.9 10.9 10.1 10.4 10.5 10.2 10.5 10.7 10.0 10.3 10.6 10.8 10.4 10.2 10.2 Bottom Start 10.6 11.0 10.6 10.5 10.5 10.0 10.1 10.5 9.6 10.4 10.1 10.1 10.4 10.6 10.2 10.0 End 10.5 10.8 10.7 10.4 10.4 10.1 9.9 10.5 10.4 10.0 9.9 10.3 10.4 10.2 10.1 9.8

  • Dally awrage Rher ftow at Holtwood.

55

Final Report PBAPS Thermal Study Table 5-6. Dissolved oxygen and water temperature measured during trawl collections in Conowingo Pond, April through October 2011.

13& 14April 2011 Flow 107,257 & 115,914 els McClellan'* Rock Below Burkin* Run Below PBAPS Broad Creek PBAPS Intake Slatlon No 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ("F)

Surf. Start 599 500 49.6 56.e 46.9 49.6 49.3 61 .7 49.S 496 51.4 52.2 50.0 500 496 466 End 57 6 496 49.3 57.4 48.7 48.7 489 604 49.6 49,5 514 52.5 50.4 496 49.6 464 Bot. Start 504 496 49.6 52.2 46.6 48.9 49.1 50.0 49,S 49,1 51 .1 51 ,4 49.8 50.0 496 466 End 511 496 46.9 55.0 46.7 48.7 48.9 538 49.6 49,5 51 .3 52.0 502 49.6 49.6 464 Dia Oxygen (mg/I)

Surf. Start 11 .2 11.4 11 .6 11 .5 11 .4 11.S 11.4 11 .2 11 .5 11 ,5 116 110 116 11.6 11 a 11 9 End 11 4 11 8 11.S 11.7 11.S 11.9 11.6 11 .6 11.9 11 ,9 11.6 117 116 120 120 12 0 Bot. Start 106 11.0 10.2 11.8 11.5 11 .4 11.2 11.7 11.S 11.6 108 102 96 119 11 7 12.0 End 11.4 11 .2 11.2 11 .8 11 .6 11 .6 11.2 12 0 11.S 11 7 10.3 104 10.6 11 9 119 12 2 Deoth !ftl 24 15 26 14 11 22 a 16 15 6 15 28 30 15 19 22 10 & 11 Mav 2011 Flow: 79 168 & 67 950 els Station No 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ("F)

Sud. Start 70.7 594 59.0 65.8 59.4 59.0 59.0 666 58.1 57.2 63.3 62.2 59.4 57.2 57.2 58.1 End 72.0 594 60.S 67.1 59.4 59.4 62.1 653 58.5 57 6 63.0 66.2 59.7 57.6 57.7 58.5 Bot. Start 59.0 590 59.0 58.3 58.6 58.6 58.6 57.9 57 2 57 2 61 .2 59.9 57.2 57.2 57.2 57.6 End 59.5 592 59,0 58.3 59.0 59.0 59.4 58 5 57.9 57 6 63.0 60.3 59.2 57.6 57.6 58.3 Dia Oxygen (mg/I)

Sulf. Start 10.2 10.4 10.5 10.4 10.S 10.6 10.8 104 10.2 10 5 10.4 10.6 10.6 10.6 10.4 10.6 End 10.2 10.6 10.5 10.S 10.9 10.9 10.7 107 10,S 10 7 10.7 10.S 10.6 10.S 10.7 108 Bel. Start 10.4 10,2 105 10.6 10.S 10.6 10.4 100 106 105 9.8 10.4 10.4 10.5 10.2 104 End 10.5 10.4 10.5 10.8 10.5 10.6 10.6 109 10 8 10.S 10.4 10.2 10.6 10.6 10.5 10.6 De<!lh (ftl 24 11 19 18 10 20 6 20 16 6 5 27 24 18 20 22 13 & 15 June 2011 Flow: 35 491 & 38 038 els Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ("F)

Sulf. Start 84.4 786 78.8 856 79.2 77.9 788 846 76.6 77.4 79.2 60.2 79.9 77.9 76.1 78 4 End 87.8 77.0 77.0 86.9 79.2 79.7 792 84 0 79.2 79.2 61 .1 80.6 80.2 78.S 78.S 788 Bel. Start 77.5 774 76.S 78.4 76.8 78.1 768 781 76.S 77.4 76.6 78.8 77.0 78.4 78.8 78 4 End 77.2 770 77.0 78.8 79.3 79.2 790 766 792 79.2 61 .1 77.9 76.4 76.8 78.8 78 8 Dia Oxygen (mg/I)

Surf. Start 8.6 8.7 8.3 8.0 8.8 8.5 90 8.0 8.4 84 7.5 9.0 6.7 6.0 7.9 8.0 End 8.8 86 7.9 8.1 8.6 9.0 90 8.2 8.3 8.1 8.7 8.7 8.5 8.1 8.1 82 Bot. Start 7.7 8.4 8.2 7.8 8.2 8.0 88 8.0 8.0 8.1 6.6 7.6 7.4 7.8 7.6 8.0 End 8.1 84 73 7.6 8.2 8.2 88 so 8.2 8.1 8.0 7.3 8.1 8.0 8.0 8,1 nAnlh!ftl 26 12 20 20 10 18 6 20 13 6 7 29 32 17 20 19 14 & 18 July 2011 Flow: 12,050 & 9, 171 cfs Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ("F)

Sulf. Start 95.4 87.S 69.2 93.4 85.6 87.3 87.4 89,6 85.1 63.S 93.6 91.8 94.1 81.1 81 .9 82.4 End 95.5 90.7 90.0 92.5 85.6 86.0 85.3 68.2 84 7 840 93.6 92.8 92.8 81.5 81 9 81 9 Bot. Start 83.3 84.2 82.8 93.4 85.6 83.8 85.6 822 851 82 8 68.7 82.8 82.0 81.0 808 82.2 End 84.6 842 85.3 85.8 82.6 83.8 84.7 864 84.7 83 5 90.0 82.4 87.8 81 .5 81 .9 81 9 Dia Oxygen (mg/I)

Sulf. Start 8.0 8.4 9.0 7.9 7.9 6.1 8.2 78 79 7.1 9.6 9.8 6.6 7.3 72 7.3 End 8.2 8.8 8.2 7.9 8.4 8.2 8.9 78 73 73 9.6 9.8 9.0 7.3 7.2 7.0 Bot. Siert 5.5 5.0 5.0 7.7 7.4 6.7 6.1 71 76 7.1 8.2 2.5 2.8 7.4 70 66 End 6.3 6.0 3.7 7.4 6.7 6.2 8.7 7.7 73 69 8.8 2.4 6.7 7.0 70 64 Deolh !ftl 24 11 19 13 8 17 4 12 6 6 8 30 30 12 16 16 Flow = Daily a181llge Rh.er ftow at Holtwood 56

Final Report PBAPS Thermal Study Table 5-6. Continued.

15 & 16 August 2011 Flow 14,667 & 13,822 els Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ("F)

Surf. Start 856 840 82.8 92.3 83.8 84.2 84.6 88.2 835 62.8 82.0 81.9 62.0 81 .0 81 .0 62.4 End 882 82.8 82.4 91.8 83.7 83.8 83.5 84.6 829 62.8 82.4 81.9 62.0 79.3 80.2 62.0 Bot. Sta1 622 842 80.1 81.0 80.6 80.2 84.6 62.4 80.2 80,6 82.2 82.0 81 .0 79.7 79.7 802 End 62.0 829 80.6 80.6 80.4 80.2 62.0 81 .9 80.2 806 82.4 81 .9 62.0 79.3 79.5 80.2 Dia Oxygen (mg/I)

Sui. Start 7.4 7.2 7.3 7.9 8.3 8.2 7.8 7.9 78 68 6.8 6.9 7.6 7.9 7.9 72 End 7.5 76 7.5 8.2 7.7 7.6 8.7 8.0 77 68 6.7 7.4 7.4 7.3 7.9 7.7 Bot. Start 68 71 6.4 7.3 7.4 7.0 7.4 7.5 72 72 6.7 7.3 6.1 7.4 7.2 68 End 66 72 6.4 7.3 7.3 6.8 8.2 7.4 68 62 6.6 7.3 6.8 6.7 7.2 70 Depth (ft) 26 NA 22 18 10 19 NA 18 12 8 7 28 34 14 15 18 19 & 20 Seotember 2011 Flow 52,035 & 44,669 els Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ("F)

Sui. Start 694 67.1 66.2 68.9 64.8 65.3 65.3 72.0 648 640 66.2 68.4 67.6 63.9 64.0 64.0 End 730 680 64.8 72.9 65.7 64.8 66.7 72.9 644 64,4 66.6 68.0 66.6 63.9 64.0 64.4 Bot. Start 644 644 64.8 64.2 64.4 64.4 65.3 64.0 65 3 630 64.4 64.4 64.6 63.9 64.0 64.0 End 644 644 64.8 64.0 64.6 64.4 64.2 64.2 644 64.4 66.6 64.4 64.6 63.9 64.0 64.0 Dia Oxygen (mg/I)

Sui. Start 10.5 104 9.6 10.6 10.4 10.4 10.2 10.4 10.4 98 10.8 10.8 9.5 10.8 11.2 10.4 End 10.2 106 10.4 10.3 10.3 10.6 8.9 10.4 10.6 10.0 10.9 10.3 10.0 120.6 10.5 10.4 Bot. Start 10.8 103 10.0 10.5 10.5 10.4 10.2 10.5 10.5 92 11.0 11.0 9.8 10.4 10.8 10.3 End 10.7 106 10.6 10.6 10.6 10.6 7.6 10.5 10.6 10.1 10.9 10.2 10.1 10.5 10.5 107

!lAnth (111 26 12 22 17 7 17 4 18 6 4 4 23 30 16 17 13 11 & 12 October 2011 Flow. 46 280 & 42 092 els Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ('F)

Surf. Start 60.6 60.4 60.4 66.4 60.6 60.4 61.2 64.2 608 613 61.3 62.4 61 .3 66.6 59.9 604 End 60.6 60.4 60.4 65.7 60.8 60.8 60.8 63.9 60.8 608 61.3 62.1 61.5 67.6 60.1 599 Bot. Sta1 60.6 60.4 60.3 67.1 60.4 60.3 60.4 60.4 61.0 61 .0 60.6 60.4 59.9 59.9 59.9 59.5 End 60.6 60.6 60.4 64.4 60.6 60.6 60.6 60.8 608 608 61.0 60.6 60.3 60.3 60.1 59.5 Dia Oxygen (mg/I)

Sui. Start 11.2 102 10.4 10.6 10.4 10.3 10.2 10.7 106 10.4 10.2 10.5 10.4 10.7 10.4 10.4 End 9.9 102 10.7 10.4 10.4 10.3 9.8 10.5 10.0 10.4 10.1 10.4 10.6 10.4 10.4 104 Bot. Start 11 .3 102 10.3 10.4 10.2 10.1 10.2 10.6 10.4 10.2 9.8 10.4 10.2 10.5 10.4 104 End 9.9 103 10.6 10.4 10.4 10.4 9.6 10.6 10.4 10.3 10.0 10.2 10.0 10.6 10.4 10.4 Deoth 1111 14 18 13 11 9 16 5 16 6 8 7 25 32 25 12 30 Flow = Daily awrage Riloef fla.v at Holtwood 57

Final Report PBAPS Thermal Study Table 5-7. Dissolved oxygen and water temperature measured during trawl collections in Conowingo Pond, April through October 2012.

6 & 11Aoril2012 Flow 27 209 & 19.766 els McClellan's Rock Below Burkina Run BelowPBAPS Broad Creak PBAPS Intake Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ("Fl SLXf. Start 64.0 55.4 532 66.2 55.0 53.6 54.9 61 .2 53.6 52.2 59.4 58.6 58.1 540 53.6 536 End 64.4 540 53.8 621 54.1 54.5 54.9 56.8 54.0 53.6 592 576 559 53.6 53.6 53.6 Bot. Start 58.6 554 53.6 57.2 55.0 53.6 54.5 54.5 54.0 52.2 59.0 586 57 6 536 53.6 538 End 56.8 541 53.6 61.7 54.3 54.0 54.9 55.4 54.0 53.6 59.2 567 54 7 536 53.6 53.8 Dia Oxygen (mg/I)

Surf. Start 11 .2 11.5 11 2 125 12.4 12.4 13.2 12.7 12 5 12.3 122 11 4 114 12.4 12.2 11.9 End 11 .2 11.2 108 12.3 12.6 13.3 12.8 12.5 130 12.3 116 11 .3 11 .0 12.4 11 .9 12 0 Bot. Start 12.0 122 12 2 12.5 13.1 12.9 13.8 12.8 126 120 124 13.4 13 2 12 5 12.1 120 End 13.0 12 3 11 .9 12.6 12.8 13.3 13.3 12.8 130 12.4 11 .5 11 .8 12 0 126 120 120 Depth (It) 24 13 19 16 9 18 4 12 5 5 7 30 27 12 18 14 25 Mav 2012 Flow: 42 258 els Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Tamp. ("F)

Surf. Start 777 68.0 71 .6 80.2 70.2 69.8 72.0 78.4 71 .6 71 .6 72.0 73.4 74.3 73.4 73.4 743 End 81 .0 70.3 71 .4 82.0 70.9 71.8 74.3 73.9 71 .6 73.2 72.9 72.9 75.0 72.9 730 73.8 Bot. Start 700 68.4 68.9 77.7 69.8 68.2 72.0 70.2 694 70.7 72.0 69.8 69.8 70.5 702 70.2 End 694 684 68.4 69.8 69.6 69.3 71.4 69.6 69.4 70.7 72.9 70.0 70.3 71 .2 711 698 Dia Oxygen (mg/I)

Surf. Start 95 96 9.2 9.5 9.8 9.4 10.5 9.5 10.0 9.5 8.8 8.6 9.4 10.2 98 10.2 End 9.6 9.6 9.6 9.4 10.0 10.7 10.2 9.7 99 10.1 8.8 9.3 9.7 9.8 10.0 10.2 Bot. Start 92 90 9.0 9.5 9.5 8.8 10.0 9.4 96 95 8.8 8.8 9.0 9.8 94 94 End 92 9.0 8.7 9.2 9.7 9.4 9.5 9.7 95 10.0 8.4 8.8 9.0 9.9 97 94 Deoth lltl 25 12 17 15 10 18 5 15 18 4 5 24 18 15 18 14 21 & 22 June 2012 Flow: 18 360 & 17 241 els Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Tamp. ("Fl Surf. Start 84.4 824 81 .0 84.6 81.0 80.8 82.2 82.4 799 80.6 82.0 82.8 82.8 77.5 78.6 788 End 86.4 81 0 82.0 82.0 80.8 82.8 84.4 81.0 78 8 80.6 82.0 82.0 83.3 77.0 77.4 790 Bot. Start 77 0 802 76.6 76.5 75.6 75.6 81 .0 76.5 752 79.2 80.8 76.6 75.6 75.4 75.2 75.6 End 77 4 792 77.9 76.5 77.0 75.6 81.7 76.3 77.2 79.5 81 .7 78.3 80.2 76.6 75.7 759 Dia Oxygen (mg/I)

Surf. Start 8.5 79 8.2 8.5 9.4 9.8 9.2 8.6 8.8 103 8.8 11 .2 10.0 10.3 92 10.3 End 84 8.7 8.7 8.8 9.0 9.0 9.8 9.5 8.6 102 8.7 9.0 8.9 7.8 90 10.4 Bot. Start 85 8.4 7.6 8.4 8.2 7.6 9.6 8.4 76 102 8.5 6.9 7.6 7.8 75 7.6 End 8.0 8.1 8.3 8.5 9.1 7.0 11 .2 8.3 8.5 106 8.7 8.2 8.6 7.2 74 75 Depth (ft) 25 11 22 22 8 19 5 18 8 5 4 22 17 13 16 14 16 & 17 Julv 2012 Flow: 6, 947 & 8, 046 els Slation No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Tamp. ("Fl Surf. Start 95.0 91.0 91 .6 93.6 887 88.5 90.0 91 .0 89.2 88.7 89.2 89.4 91 .4 84.6 86.7 87.4 End 95.2 89.4 90.7 91 .2 896 90.0 90.5 89.4 89 2 88.0 89.2 90.9 91 .8 86.0 86.7 86,9 Bot. Start 86.4 89.6 84.0 87.8 87 8 84.2 90.0 86.9 85.6 88.2 89.1 86.4 82.2 846 83 3 84.6 End 85.5 842 83.8 855 85.5 83.8 89.8 86.0 86.0 87.3 89.1 86.0 88.2 84 0 83 7 85.6 Dia Oxygen (mg/I)

Surf. Start 8.5 8.0 8.5 7.9 8.2 7.9 8.0 8.1 81 8.1 7.8 8.0 8.2 8.0 80 8.1 End 8.7 9.2 8.7 8.2 8.4 8.2 8.7 8.3 7.9 79 7.7 8.4 8.3 8.7 86 84 Bot. Start 3.0 6.7 4.0 74 75 5.8 7.6 8.0 6.5 80 7.0 2.3 0.6 7.4 60 61 End 6.8 5.1 4.3 66 58 50 8.4 7.5 6.4 72 7.4 1.7 5.9 6.8 63 70 Death Cftl 26 12 22 18 9 18 5 13 10 6 5 27 25 13 16 12 Flow = Daily awrage Ri.,.,, flow et Holtwood 58

Final Report PBAPS Thermal Study Table 5-7. Continued.

13 & 14 August 2012 Flow: 8,514 & 9, 014 els Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ('F)

Surf. Start 92.8 88.0 88.2 94.1 87.8 89.8 90.0 90.5 88.4 87.4 87.4 88.2 88.9 84.4 84.9 85.8 End 93.8 87.1 87.8 90.1 88.7 89.8 90.1 87.8 88.5 85.8 87.3 87.3 87.4 83.8 83.7 84.9 Bot. Start 85.1 88.0 84.2 88.9 84.6 83.6 89.2 85.6 84.2 85.8 88.9 85.8 84.2 83.3 83.3 85.1 End 84.2 83.7 87.8 65.5 85.3 83.3 88.5 85.5 85.8 65.8 87.3 85.5 67.3 83.5 82.8 83.3 Ola Oxygen (mg/I)

Surf. Start 7.2 8.8 8.6 7.5 7.8 7.6 7.8 7.8 7.6 7.4 5.9 6.6 7.0 7.8 8.0 7.2 End 7.0 8.7 8.8 8.0 7.8 7.3 9.4 7.9 7.2 7.8 8.3 8.8 7.2 7.7 8.0 7.9 Bot. Start 5.0 8.2 3.8 7.0 5.4 4.5 7.9 7.2 5.2 8.8 5.8 4.0 3.2 7.5 8.8 7.0 End 5.8 5.3 5.8 7.2 5.3 4.3 13.6 7.5 6.4 7.8 8.1 3.8 8.4 7.8 7.1 5.6 ln..nth {ft) 24 13 22 17 9 19 5 13 7 5 5 28 22 15 17 15 10& 11 Seotember2012 Flow: 10,070 & 10.012 els Slatlon No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ('F)

Surf. Start 82.6 82.4 80.8 84.2 80.8 78.3 79.7 78.4 78.8 78.4 81.5 82.0 81.0 74.8 75.6 75.9 End 83.7 82.6 81.5 82.2 81.1 78.3 78.8 77.4 78.4 77.4 81.3 82.0 81.9 74.8 75.8 76.5 Bot. Start 82.2 81.5 81 .5 82.4 81.0 77.0 79.3 75.9 76.8 73.2 81 .5 80.8 82.0 75.2 75.4 75.4 End 82,4 82.8 81 .5 79.2 81.3 77.0 74.3 78.6 78.8 78.3 81.3 82.0 81.9 75.2 75.8 75.8 Dia Oxygen (mg/I)

Surf. Start 8.0 7.9 8.0 8.2 8.4 9.2 9.5 8.4 9.0 8.9 6.4 7.4 7.0 7.6 7.3 7.8 End 7.9 8.1 8.0 8.3 8.2 9.2 11 .6 8.5 8.7 8.8 8.9 7.7 7.9 7.2 7.4 7.8 Bot. Start 7.7 7.5 7.9 7.3 8.8 7.5 9.2 7.7 7.9 5.4 4.6 7.5 7.0 7.3 7.1 7.2 End 7.1 8.0 7.6 8.8 8.3 7.1 10.8 7.9 7.8 8.0 6.8 7.8 7.4 8.9 7.2 8.9 IDeoth Cftl 25 11 21 17 9 17 5 15 11 5 5 25 18 14 16 14 8 & 9 October 2012 Flow: 13 256 & 12 229 els Station No. 331 332 333 381 382 383 384 371 372 373 341 342 343 321 322 323 Water Temp. ('F)

Surf. Start 70.0 63.1 84.0 71 .2 84.4 65.3 88.2 71.2 84.4 84.8 84.9 88.0 84.8 63.5 84.4 64.2 End 71 .2 63.5 63.9 70.2 84.2 84.4 84.6 68.0 83.9 84.4 68.4 88.8 65.7 63.9 84.4 64.4 Bot. Start 84.0 84.0 84.0 85.3 84.4 64.8 88.2 84.4 64.4 84.8 84.9 65.3 84.4 84.0 84.4 84.2 End 63.9 63.5 63.9 84.4 84.4 84.4 84.4 84.8 84.0 84.4 66.6 64.8 65.1 84.0 84.4 84.4 Ola Oxygen (mg/I)

Surf. Start 6.8 8.4 8.6 8.5 8.8 6.4 8.0 8.8 8.5 8.2 8.2 8.5 8.2 8.5 8.6 8.5 End 8.3 8.2 8.1 6.7 8.5 6.4 8.3 8.5 8.7 8.1 6.3 8.5 8.4 8.6 8.4 8.3 Bot. Start 8.2 8.1 7.6 8.0 8.1 8.2 7.8 7.9 8.2 7.8 7.5 8.3 6.0 8.4 8.2 7.9 End 8.0 7.9 7.8 7.8 8.3 7.7 7.9 8.3 8.2 7.7 8.2 7.8 7.9 8.4 8.2 8.1 Deoth (ft) 25 10 28 16 9 20 5 15 10 7 5 28 25 16 18 14 Flow = Daily alo9lllga Rher ftow at Holtwood 59

Final Report PBAPS Thermal Study 11.0 SURFA.CEDO 10 0 9.0 8.0

~

g 70 0

0 6:0 so

- Fishing Crtek -Burkins Run

- Willizms Tu1111el -S!a!tLint 40

!OJun 4Jul  !!Jul lSJul 25Jul lAlJE 8Alll! 15Au!! 22AUJ! l9Sep 240ct 1999 (Week oO 1:!.0 . . . - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - .

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Figure 5-19. Dissolved oxygen measured at the surface and at the bottom at four locations in Conowingo Pond, June to October 1999. Reproduced from Normandeau Associates 2000.

60

Final Report PBAPS Thermal Study Table 5-8. Selected weekly DO profiles at transect locations 0N =western area; M = mid-pond; and E = eastern area) in Conowingo Pond, June-October 1999. Reproduced from Normandeau Associates 2000.

Week or 2Q.Jun II-Jul 25-Jul S.Auc 22-Aug 19-Sep 24-0ct Depth W M E W M E W M E W M E W M E W M E W M E Fuhing Cruk 86 88 94 6 7.3 8.4 80 80 74 68 82 82 66 69 72 87 82 81 10 I 100 100 70 86 5.9 7.3 8.4 70 79 69 82 65 69 86 82 JOO 99 100 10 66 77 5.9 7.1 8.2 67 77 69 79 64 85 82 JOO 99 15 63 5.8 69 64 10 0 Bottom 60 5I 10.2 5.1 7. 1 8.1 6.2 56 73 69 66 81 64 58 71 85 82 81 100 100 99 Burkim Run 76 83 8.3 7.1 7.1 6.9 71 64 7I 75 86 72 71 73 82 82 81 99 98 IOI 77 65 7.1 72 6 I 69 71 68 8.2 82 99 97 10 78 7.1 6.4 70 8.0 8J 99 97 15 73 Bottom 79 51 68 7.1 6.1 6.9 7I 5J 6.0 7I 66 70 6,0 64 8.0 78 80 99 97 10 I Wil/iamJ Tunnel 71 72 74 7. 1 6.8 6.9 6.8 69 71 84 7I 72 72 84 85 86 98 97 98 6.8 70 73 6.8 6.7 6.8 6.6 68 68 86 8 88 68 6_9 71 8.4 85 86 97 97 98 10 61 69 71 6 6.5 6.6 6.3 61 59 78 8I 67 69 6.9 8.4 83 86 96 96 97 15 58 5I 64 6.2 47 36 45 65 67 85 86 96 95 97 20 48 5.6 27 54 85 96 25 I0 4.6 22 85 96 Bottom 34 40 35 4.5 5.9 3.7 29 32 12 6.1 4I 53 80 82 83 9.7 95 95 PAIMD Sta1t line 87 83 77 6.7 6.6 72 66 70 94 86 87 74 72 72 85 87 87 94 96 95 85 s2 11 6.7 6.6 6.5 69 61 68 85 86 73 72 71 84 86 86 94 96 95 10 80 85 74 66 6.6 6J 64 59 61 79 76 72 70 70 83 84 86 94 95 95 15 77 65 58 64 61 62 55 69 64 72 6.4 66 85 81 86 93 95 95 20 53 40 61 33 40 J9 61 85 92 94 25 29 61 16 3 I 6.0 85 94 JO 24 44 16 35 55 84 94 35 2.2 43 06 39 85 93 40 20 41 0I 40 83 93 Bottom 25 58 19 54 64 J9 32 44 14 35 68 39 5J 55 4.3 8.3 80 82 92 95 93 61

Final Report PBAPS Thermal Study 5.4 Shoreline Habitat Introduction In considering the potential effects of the PBAPS thermal discharge, it is necessary to understand not only the distribution of the thermal plume but the types of aquatic habitats that experience elevated temperatures. To facilitate evaluation of potential thermal effects on benthic macroinvertebrates and fish in shallow shoreline habitat, the amount of shallow shoreline habitat in the non-thermally and thermally affected areas were quantified. Shallow shoreline areas are important habitats for both the benthic macroinvertebrates and fish within Conowingo Pond.

For this study, the benthic macroinvertebrate community was assessed for only the wadeable shoreline habitats in the Pond, specifically to characterize the composition and abundance of organisms within this habitat type. Similarly, the fish community that used the shallow shoreline habitats was characterized by both electrofishing and seining. This study did not evaluate the much more extensive benthic macroinvertebrate habitats or communities in the deeper offshore areas of the Pond. However, the fish community residing on the bottom of the Pond in offshore areas was assessed using a bottom trawl. The thermal monitoring and modeling has shown that elevated water temperatures are primarily a surface phenomenon in the open water portions of the Pond and along the west shoreline areas in close proximity to the PBAPS discharge canal.

This is why the focus of the habitat analysis is on the shallow shoreline areas.

Methods The shallow shoreline habitats were quantified within the impounded portions of Conowingo Pond from the upper end of Lower Bear Island, which is in the vicinity of MRPSF, downstream to Conowingo Dam (Figure 5-21). This analysis excludes the shallow shoreline areas upstream from Lower Bear Island where the waterbody is 01ore characteristic of a free-flowing riverine system and also excludes the mouths of tributary streams. GIS was used along with the bathymetry dataset developed for the Conowingo Hydroelectric Facility relicensing project to quantify the shoreline habitats (URS 2011 ). For the purposes of this analysis shallow habitats were defined as those that were less than or equal to 10 feet in depth at the maximum Pond elevation of 11 O feet, which approximates the maximum water level for the Conowingo Pond.

No attempt was made to determine the quality of shallow shor!31ine habitat, rather, the focus was to quantify the approximate areas of this type of habitat in the Pond. It is clear from field observations that the quality of shallow shoreline habitat is variable with portions of the shallow shoreline habitat having steeply sloping banks that are likely a less productive type of benthic macroinvertebrate habitat.

Results The total water surface area in the Pond, as used in this analysis, is approximately 8,327 acres with 3,593 acres upstream from the end of the PBAPS discharge canal and 4,734 acres downstream from the discharge canal (Figure 5-20). This total includes approximately 488.2 acres of shallow shoreline between elevation 110 and 100 feet (Table 5-9). A total of 306.8 62

Final Report PBAPS Thermal Study acres of shallow shoreline habitat occurs upstream from the PBAPS discharge canal and is not significantly affected by the thermal plume. Areas downstream that are potentially affected by the thermal plume total 181 .1 acres. Most of the shallow shoreline habitat in the Pond, as determined in this analysis, is concentrated in the upper portion or along the eastern shoreline.

A small portion of this shallow shoreline habitat occurs within close proximity of the PBAPS discharge canal (Figure 5-21). The amount of shallow shoreline habitat from the end of the discharge canal to Station 215 is approximately 12 acres (Table 5-10). This is the primary area of potential thermal impact to both benthic organisms and fishes. The amount of shallow shoreline habitat from Station 215 downstream to Station 189 is 7.3 acres (Table 5-11).

Discussion The shallow shoreline habitat analysis indicates that Conowingo Pond contains generally steep shorelines with relatively small amounts of shallow shoreline. Shallow shoreline habitat comprises a small proportion (5.86%) of the total Conowingo Pond surface area from the vicinity of MRPSF to Conowingo Dam. Greater amounts of shallow shoreline habitat are present upstream of the PBAPS discharge canal as compared to downstream. These upstream habitats are unaffected by the thermal plume except the vicinity of Station 208 is occasionally thermally affected at low River flows and concurrent pump up operation of MRPSF. Shallow shoreline comprises approximately 8.5% of the total surface area in Conowingo Pond that is present upstream from the PBAPS discharge canal. In contrast shallow shoreline comprises only 3.8% of the Pond total surface area that is located downstream of the PBAPS discharge.

Limited shallow shoreline habitat is present directly downstream from the discharge canal in the primary area of potential thermal impact. Thus, only a small amount of habitat is exposed to the highest temperature water from the PBAPS discharge before the thermal plume mixes with ambient temperature water and disperses and moves offshore primarily on the surface of the Pond.

The primary area of potential effect comprises less than 19 acres of the total shallow shoreline habitat. Subsequent sections of this chapter evaluate benthos and fish community impacts observed within these shallow shoreline habitats. The 19 acres of potential shoreline habitat effect is conservatively high because this was calculated at maximum pool elevation and includes areas that may be dry during summer and other times of the year. The combination of operation of MRPSF and Conowingo Hydroelectric facility results in fluctuations in Pond elevation throughout the course of the year. The annual average water elevation for the Pond during 2004 to 2010 was 108.1 ft (URS 2011 ). Also, the Federal Energy Regulatory Commission (FERC) license for the Conowingo Hydroelectric Project permits a minimum Pond elevation of 101 .2 ft which would expose most of the shallow shoreline habitat within the near-field impact zone.

The location of the PBAPS discharge on the west shore and in the middle section of Conowingo Pond is advantageous in terms of reducing the amount of shallow shoreline habitat exposed to the highest temperature water. The design of the jet discharge is also important as it rapidly entrains ambient water into the plume, thus quickly diluting the high temperature water from the discharge canal.

63

Final Report PBAPS Thermal Study

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Final Report PBAPS Thermal Study Elevation Range 110*109 109-108 108-107 107-106 106-10~

10~104 104-103 103-102 102*101 101-100 0 500 Figure 5-21. Shallow shoreline habitat in the vicinity of the PBAPS discharge canal.

65

Final Report PBAPS Thermal Study Table 5-9. Amount of shallow shoreline habitat in Conowingo Pond from vicinity of MRPSF downstream to Conowingo Dam.

Conowingo Pond Water Depth Shallow shoreline habitat 2 1 Elevation (1 ft intervals) (feet) Acres Total acres at Elevation  % of Total Pond Surface Area 110-109 1 11.9 488.2 5.86 109-108 2 12.9 476.3 5.72 108-107 3 19.2 463.4 5.56 107-106 4 55.1 444.2 5.33 106-105 5 88.6 389.2 4.67 105-104 6 63.7 300.6 3.61 104-103 7 70.2 236.9 2.85 103-102 8 68.0 166.8 2.00 102-101 9 52.6 98.8 1.19 101-100 10 46.2 46.2 0.55 1

Total surface area of Conowingo Pond from vicinity of MRPSS to Conowingo Dam is 8327.6 acres Total surface area of Conowingo Pond from Holtwood Dam to Conowingo Dam is 9,000 acres 2

Total shallow shoreline habitat for areas lOft or less in depth at various elevations, shoreline area derived from URS bathymetry dataset which includes shallow shoreline areas within 50ft of islands but not shallow areas within the main channel Table 5-10. Amount of shallow shoreline habitat from the end of the PBAPS discharge canal downstream to Station 215.

Conowingo Pond Elevation Total acres at  % ofTotal Pond  % ofTotal Pond (1 ft intervals} Acres Elevation Surface Area1 Shoreline Area 2 110-109 0.56 11.64 0.14 2.39 109-108 0.38 11.09 0.13 2.27 108-107 0.47 10.71 0.13 2.19 107-106 0.74 10.24 0.12 2.10 106-105 1.22 9.50 0.11 1.95 105-104 1.67 8.28 0.10 1.70 104-103 1.75 6.61 0.08 1.35 103-102 1.82 4.86 0.06 1.00 102-101 1.55 3.04 0.04 0.62 101-100 1.49 1.49 0.02 0.31 1

Total surface area of Pond from vicinity of MRPPS to Conowingo Dam is 8327.6 acres 2

Total shallow shoreline habitat is 488.2 acres for areas lOft or less in depth at various elevations; shoreline area derived from derived from URS bathymetry dataset which includes shallow shoreline areas within 50ft of islands but not shallow areas within the main channel not adjacent to land 66

Final Report PBAPS Thermal Study Table 5-11. Amount of shallow shoreline habitat from Station 215 to Station 189.

Conowingo Pond Elevation Total acres at  % of Total Pond  % ofTotal Pond 1 2 (1 ft intervals) Acres Elevation Surface Area Shoreline Area 110-109 0.18 7.32 0.09 1.50 109-108 0.22 7.14 0.09 1.46 108-107 0.29 6.92 0.08 1.42 107-106 0.42 6.63 0.08 1.36 106-105 0.78 6.22 0.07 1.27 105-104 1.08 5.44 0.07 1.11 104-103 1.10 4.35 0.05 0.89 103-102 1.12 3.25 0.04 0.67 102-101 1.08 2.13 0.03 0.44 101-100 1.05 1.05 0.01 0.21 1

Total surface area of Pond from Muddy Run station to Conowingo Dam is 8327.6 acres Total surface area of Pond from Holtwood Dam to Conowingo Dam is 9,000 acres 2

Total shallow shoreline habitat is 488.2 acres for areas lOft or less in depth at various elevations; shoreline area derived from URS bathymetry datasetwhich includes shallow shoreline areas within 50ft of islands but not shallow areas within the main channel not adjacent to land

5. 5 Benthic Macroinvertebrate Community A study of the benthic macroinvertebrate community was conducted to determine the influence of the thermal plume on the composition and relative abundance of the benthic macroinvertebrate, or benthos, community inhabiting shallow-water shoreline habitat in Conowingo Pond. Previous benthos surveys conducted relative to PBAPS have evaluated the benthic macroinvertebrates residing in deeper, off-shore habitats in the Pond. This is the first survey of benthos in the nearshore habitat. The benthic macroinvertebrate sampling included an assessment of habitat quality at each of the collection locations.

Methods Habitat Assessment The quality, quantity, and variety of physical habitat are well-known determinants of macroinvertebrate community composition. When comparing sample stations, habitat assessments are used to infer whether observed differences in macroinvertebrate communities are the result of water quality degradation (in this case, increases in temperature) or due to variations in habitat. The PADEP-approved methodology used for this study is adapted from one described in USEPA (1999) for low gradient (glide pool) streams. The methodology involves visual inspection and quantification of nine habitat parameters:

  • Epifaunal Substrate/Available Cover
  • Channel Alteration
  • Pool Substrate Characterization
  • Bank Stability
  • Pool Variability 67

Final Report PBAPS Thermal Study

  • Bank Vegetative Protection
  • Sediment Deposition
  • Riparian Vegetative Zone Width
  • Channel Flow Status Each is awarded a score between 0 and 20 for a possible maximum total of 180. The resulting values can be used to rate habitat quality as follows:

Optimal 166-180 Sub-optimal 113-153 Marginal 60-100 Poor <47 Scores falling between these ranges are given a dual rating. For example, a score of 112 at Station 215 reported herein is described as sub-optimal/marginal.

Macroinvertebrate Collection and Analysis Macroinvertebrates were collected monthly with a D-frame kick net according to a PADEP (2007) multi-habitat protocol at most of the same locations utilized for the seine collections (Figure 5-22).

Each multi-habitat sample was a composite of 1O "kicks," collected from five habitat types:

  • Cobble/gravel,
  • Snag,
  • Coarse particulate organic matter (CPOM),
  • Submerged aquatic vegetation (SAV), and
  • Sand/fine sediment.

Where all five habitat types were present, two "kicks" were taken from each to produce the composite. If one or more habitat types were absent, the "kicks" that would have been assigned to them were proportioned according to the predominant habitat types remaining. These samples were collected in an upstream to downstream direction.

The initial project design prepared for the 2010 study-year utilized seven sample locations. Two stations, 214 and 215, were established within the influence of the thermal plume and the remaining five were in areas upstream of the thermal discharge within the Pond. The 201 O samples were collected during the months of July through October when none of the helper cooling towers were operating.

Beginning in 2011, two new sample locations (Stations 216 and 217) within the influence of the thermal plume but farther down-river near the Maryland border were added. The PADEP 68

Final Report PBAPS Thermal Study requested these in order to determine whether the influence of the thermal plume on the benthic community was more spatially extensive than previously anticipated. Monthly sampling at these stations began in June 2011 . The seven original locations were sampled monthly from April through October.

A tenth location was added in 2012 (Station 189). This station corresponds to electrofishing Station 189 and is located within the plume, along the west shoreline, approximately 1.3 miles downstream from the outfall. It is nearer the discharge point than Stations 216 and 217 but farther away than Stations 214 and 215. Station 189 was selected to further define the extent of thermal impact attributable to the discharge both spatially (distance from the outfall) and seasonally. The hypothesis being tested was: If impact to the benthic community is occurring in July and August when ambient temperatures were the highest, then this should be reflected in comparatively lower IBI scores. If IBI scores were consistent through summer months and into the fall, then this would indicate that the limit of seasonal impact was farther upstream. All ten stations were sampled from April through October in 2013.

All samples were preserved in the field with isopropanol and transported to Normandeau Associates' laboratory in Stowe, PA for processing and analysis. At the laboratory, the sample matrices were placed into a pan divided into twenty-eight 2-inch by 2-inch grids. Specimens were removed from a minimum of four randomly selected grids until a count of 200 (+/- 20 %)

was obtained. If a sample did not contain at least 160 specimens, the matrix was processed in entirety. Specimens were sorted by type and placed into glass vials for identification.

Macroinvertebrates were identified to the genus level of scientific classification (referred to as taxa) except for midges, identified to the family level (Chironomidae), and worms, identified to class (Oligochaeta). Each taxon was then assigned a tolerance value from a list provided by PADEP. Tolerance values range from O to 10 where numbers between O and 3 indicate pollution sensitive taxa (low tolerance). Tolerance values from 4 to 6 may be interpreted to be indicative of facultative taxa. Tolerance values of 7 or greater indicate pollution tolerant taxa.

The resulting data were condensed to six ecological metrics developed by PADEP (2007). The metrics are:

  • Total Richness,
  • EPT Richness,
  • Beck's 4 Index,
  • Shannon Diversity,
  • Mayfly Taxa Richness, and
  • Caddisfly Taxa Richness Macroinvertebrate Metric Scoring The PADEP (2007) multi-habitat protocol used in this study was developed for determining water quality impairment based on composition of the benthic community in low gradient streams as compared to a reference set of high quality low gradient streams in Pennsylvania.

Although this protocol was not developed for use in reservoirs such as Conowingo Pond or designed to address benthic community impacts associated with elevated temperature, it was 69

Final Report PBAPS Thermal Study used in this study to compare the sample stations metric values and 181 scores because a more suitable protocol specifically developed for impoundments or lentic waterbodies is not yet available for Pennsylvania waters.

Benthic macroinvertebrate community composition varies depending on the type of waterbody (lentic, lotic, or tidal) and the type of habitat being surveyed. In Conowingo Pond the benthic community is characteristic of a lentic community. That is, most of the benthic organisms in shallow shoreline habitat are adapted to pool and edge habitats characterized by low current velocity. The habitat alteration due to impoundment of the Susquehanna River to create Conowingo Pond has created a more homogenous environment with small amounts of shallow shoreline habitat and shoreline habitats that are lacking habitat complexity. Most of the available benthic habitat in Conowingo Pond lies within the deeper open-water areas where the river bottom is fairly homogenous and composed of finer substrate types (sand, silt, and clay).

Nonetheless, the protocol's 181 scoring system provides a tool for making comparisons among sample stations.

As specified in the protocol, a set of equations was used to produce standardized scores for each metric that were in-turn used to produce an 181 value for each station. The 181 is a means to integrate information from the metrics into a station score ranging between O and 100. To accomplish this, some form of standardization is needed. According to the protocol, the metric values are divided by the 95th percentile of values generated from a broad data set obtained by PADEP to develop the 181:

Metric Standardization Metric Standardization Richness observed value I 31 Shannon Diversity observed value I 2.43 EPT Richness observed value I 17 MayflyTaxa observed value I 6 Beck's 4 Index observed value I 22 Caddisfly Taxa observed value I 11 As noted above, this protocol compares the Conowingo Pond community to a reference set of high quality low gradient streams in the Commonwealth. Thus, relatively low 181 scores can be expected for the benthic macroinvertebrate stations sampled in this study due to fact that Conowingo Pond is an impoundment.

The maximum value any standardized metric score can attain is 1.0. The 181 is calculated by simply taking the average of the six standardized scores and multiplying by 100. The higher the resulting 181 score, the more closely the data are to attaining a reference stream condition used to develop the protocol. According to the protocol, an 181 of 55 or more indicates that a station meets the Aquatic Life Use Designation assigned to the stream. In this study, the 181 threshold score of 55 is not appropriate for making this decision due to the impounded habitat. For the purposes of this study the 181 scores are only used to compare stations.

70

Final Report PBAPS Thermal Study A brief summary of the metrics and whether their values increase or decrease in response to water or habitat quality degradation is provided in Table 5-15.

Statistical Analyses The non-parametric Kruskal-Wallis test was used to determine whether statistically significant differences (p-value s 0.1) in IBl scores or metric values existed among the monthly collections at each sample station. If the Kruskal-Wallis test yielded significant differences then the Kruskal-Wallis multiple comparisons test was used to determine which stations differed from each other. This nonparametric test was selected for these analyses over the analogous parametric ANOVA test because not all test groups met the assumptions of equal variances, normal distribution, and there were sample size differences among the stations. The nonparametric test was used for all analyses to streamline statistical analysis among the test metrics.

Habitat Assessment Results and Discussion The results of the habitat assessment are provided in Table 5-16. Station scores ranged from 75 to 113 producing similar descriptors of sub-optimal/marginal or marginal at each location.

Placed into context, the habitat constraints observed in the Conowingo Pond are essentially due to channel alteration inherent to impoundment; i.e., a free-flowing section of the Susquehanna River has been transformed into a reservoir where shoreline habitat is much less varied and the current is much slower than it would be in a natural state. This habitat alteration would be expected to produce a negative response in what was initially a riverine benthic community; one which should be, and is, characterized by low IBI scores. Because the station scores show habitat quality to be similar at each sample location, differences in the benthic community resident in the thermally influenced versus the non-thermally influenced locations may be considered, in part, attributable to temperature increase. However, other habitat features such as the amount of submerged aquatic vegetation (SAV), water velocity, and spatial location in reference to tributaries or other Pond features are not accounted for in the habitat assessment.

Macroinvertebrates Results Four years of study have produced a total of 108 benthic macroinvertebrate taxa from the study area. The composition and abundance of benthic macroinvertebrates was similar for each year of the study. Common macroinvertebrate taxa (>1% of total organisms) were similar among collection locations and varied from 5 to 12 taxa among stations and years (Table 5-17 through Table 5-20). A few benthic macroinvertebrate taxa comprised a large proportion of all organisms collected at each of the benthos monitoring stations. With few exceptions, Chironomidae and Oligochaeta were among the most abundant organisms for all stations and years (Table 5-17 through Table 5-20).

71

Final Report PBAPS Thermal Study Other common organisms at select stations or year of collection included Corbicu/a, Stene/mis, Gammarus, and Caenis. Corbicula or Asiatic clam was introduced in the 1980s and was not observed in the Pond prior to 1980. No Plecoptera (stoneflies) and few Ephemeroptera (mayflies) or Trichoptera (caddisflies) were collected in high abundance. The mayfly Caenis was the only mayfly or caddisfly collected in relatively high numbers among years or stations. Other Ephemeroptera and Trichoptera that comprised >1 % of total organisms included Callibaetis, Stenacron, Oecetis, Hexagenia, Orthotrichia, and Maccaffertium. Total richness of common macroinvertebrate taxa combined for all stations was also similar among years, ranging from 18 to 25 taxa (Table 5-17 to Table 5-20). Similarly, EPT richness of common macroinvertebrates combined for all stations varied among years, ranging from 4 to 9 taxa. There were some observed differences in composition of common taxa among stations. Fewer common taxa

(>1% of total organisms) were collected at Station 214 in 2010-2012 as compared to the other locations. The number of common taxa collected at Station 214 in 2013 was similar to the other locations (Table 5-20). Chironomidae comprised a greater proportion (52-67 %) of the benthic community at Station 214 in 2010-2012 as compared to the other stations (Table 5-17 through Table 5-19). However, in 2013 Chironomidae abundance at Station 214 was similar to most of the other locations. Corbicula were more abundant at Stations 214 and 215 than at most of the other locations and Gammarus abundance was typically lower at Stations 214 and 215 than at the other stations.

A reduction in benthic macroinvertebrate diversity and evenness was evident during July and August at Station 214 in 2010-2012 (Table 5-21). In contrast, in 2013 diversity and evenness was higher. Three or 4 taxa comprised most of the organisms that were collected in 2010-2012 as compared to 7 or 8 taxa in 2013. Chironomidae were numerically dominant, comprising 65 and 80% of all organisms collected during July and August of 2010-2012, respectively.

Chironomidae abundance in 2013 for July and August was lower ranging from 33 to 46%.

Corbicu/a and Oligochaeta were also more abundant in 2010-2012 as compared to 2013. No Trichoptera and two Ephemeroptera (Caenis and Callibaetis) were collected in July and August.

2010-2012. In contrast, during 2013 four Trichoptera and three Ephemeroptera taxa were collected.

Summary metrics calculated for each station based on all years of data collection are presented in Table 5-22. The metrics Total Richness, EPT richness, Percent Chironomidae, HBI, Percent Sensitive Taxa, and Percent Oligochaeta were selected to describe the overall benthic macroinvertebrate community observed at each location. Most metric values were similar among stations. Note that Station 189 (N=11 monthly samples) and Stations 216 and 217 (N=19 monthly samples) include fewer monthly collection events compared to the other stations which results in fewertaxa being observed. Total richness ranged from 41 taxa at Station 189 to 65 taxa at Station 220. Richness at Station 214 was lower than all locations with the same number of samples. Similarly, EPT richness ranged from 11 taxa at Station 217 to 19 taxa at Stations 220 and 215. Otherwise, EPT richness was similar among stations. Percent Chironomidae was similar among most stations with the highest value observed at Station 214 (52.1%). HBI values were similar among stations with lowest value of 5.4 observed at Station 189. Percent sensitive taxa (tolerance value 0-3) was low for all stations with the highest value 72

Final Report PBAPS Thermal Study at Station 216 (2.6%) and lowest at Station 221 (0.2%). Percent Oligochaeta varied from 3.6%

at Station 189 to 20.7% at Station 216 with all other station values greater than 8%.

/Bl Scores 181 scores were low for all stations and years within and outside of the thermal plume (Figure 5-26). The lowest 181 scores were observed at Stations 214 (thermal) and 221 (non-thermal).

However, 181 scores at the other thermal and non-thermal stations were similar. Other slight spatial differences were observed both between and within non-thermal and thermal station groups. Some variation was observed among years with higher scores observed during 201 O or 2013 for most locations (Figure 5-27 and Figure 5-35). Note that sampling was limited in 201 O to only July-October and scores tended to be lower in April, May, and June for most stations.

Median 181 scores for Station 214 were significantly lower (p<0.05) than all non-thermal and thermal stations except non-thermal Station 221. The only other statistically significant differences in 181 scores were observed between Stations 216 and 221, with scores lower for Station 221 (non-thermal) as compared to Station 216 (thermal).

181 scores also varied seasonally with higher values observed in the fall as compared to the spring for most locations (Figure 5-28 through Figure 5-36).This seasonal pattern was quite apparent for the combined scores observed for all upstream stations (Figure 5-36). 181 scores tended to increase over the course of the field season with the lowest values observed from April to June and highest values observed from August to October. This pattern was not observed at Station 214 with scores in August to October tending to be similar to April through June. Station 215 181 scores tended to follow the pattern observed at the upstream stations with the exception of August where scores were lower for several of the collections.

Individual metrics that comprised the 181 scores were also evaluated for each monthly collection.

Figure 5-29 through Figure 5-34 show the spread of the metric values for each station. For total richness the interquartile ranges overlapped for all stations except Station 214 and greater variability was observed for Stations 202, 203, and 221 (Figure 5-29). EPT richness values were generally low with wide interquartile ranges for most stations ranging from Oto 8 taxa among stations (Figure 5-30). EPT richness values were lowest for Stations 214 and 221. Similar to EPT richness, Ephemeroptera richness values were low and variable ranging 0 to 6 taxa among stations (Figure 5-31). Fewer Ephemeroptera taxa were collected at Stations 214 and 221. Few Trichoptera were collected, as indicated by low richness values for all stations with the highest richness observed at Station 208 (Figure 5-32). Beck's Index values were similar among stations with the highest values observed at Stations 189 and 216 and lower scores at Station 214 (Figure 5-33). Shannon diversity was remarkably similar for all stations with interquartile ranges overlapping for all stations; however, values were generally lower for Station 214 (Figure 5-34).

Similar to 181 scores, individual metric values were lower at Station 214 as compared to the other stations. Station 214 metric values were statistically different (p<0.05) from at least one other station for all six metrics (Table 5-24). Station 215 metric values were similar to both non-thermal and thermal stations. Few significant differences were observed for Station 215 metric values in comparison to all other stations. Trichoptera richness was low at Station 215 as 73

Final Report PBAPS Thermal Study compared to Station 208. Other statistically significant differences were observed between both individual non-thermal and thermal stations (Table 5-24).

Table 5-25 through Table 5-30 provide mean metric scores for each station by month of collection. Total richness was generally highest in August and September and the lowest during April and May for most stations. This general pattern was not observed at Station 214 with the lowest mean richness values at this station observed in August and highest observed during April. Similarly, mean EPT, Trichoptera, and Ephemeroptera richness were generally highest in August and September and lowest in April and May. Values of these three metrics were generally low for Stations 214 and 221, regardless of collection month. Mean Shannon diversity values were similar among most stations with the highest values observed for most stations in August through September. Mean Shannon diversity values for Station 214 were lower than all other stations during August through October and during other months within the range of values observed among the other stations. Mean Beck's Index values showed no consistent seasonal pattern with values quite variable among stations and months. However, Station 214 mean Beck's Index values were lower than other stations during July, August (tied with Station 215), and October and during other months within the range of values observed among the other stations.

Discussion Most of the macroinvertebrate taxa collected in this study are lentic (prefer slow current) forms that may be considered either facultative (tolerance value = 4 - 6) or tolerant (tolerance value =

7 - 10) of water/habitat quality degradation. Few intolerant forms (tolerance value 0-3) were collected. The observed taxa are representative of a warmwater aquatic community in a lentic waterbody. The most abundant groups were Chironomidae and Oligochaeta. Many taxa within these groups are adept burrowers found in depositional areas.

Other common genera such as Gammarus, Gyrau/us, Callibaetis, Enal/agma, Oecetis, and Orthotrichia are associated with aquatic vegetation. Other taxa such as Corbicu/a, a filter feeding clam, show a potential affinity for the warm water and/or current introduced from the PBAPS discharge.

Station 214, located about 0.35 miles below the discharge canal, is the benthic macroinvertebrate station located closest to the end of the discharge canal. The IBI scores for Station 214 were lower than the other non-thermal and thermal stations, indicating benthos effects attributable to the heated effluent. Station 215 is the next closest station to the PBAPS discharge canal and is located 0.65 miles downstream of the canal. IBI scores at Station 215 were not significantly different from the other thermal or non-thermal stations. However, lower IBI scores were observed at this station during July and/or August.

The observations indicate that the area of potential effect to the benthic community is restricted to a narrow band of shallow-water habitat along the western shoreline. Metric and IBI scores indicate that the thermal effect to the benthos community from the PBAPS thermal plume is confined to the western shoreline at Stations 214 and 215. Low IBI scores were observed at Stations 214 and 215 during July and/or August when water temperatures were the highest 74

Final Report PBAPS Thermal Study (Figure 5-4 , Figure 5-5, Figure 5-36). Improvement in both 181 scores and metric values was observed during subsequent months, indicating re-colonization and recovery of the benthic community. 181 scores and metric values at Stations 214 and 215 during the spring collections are comparable to the upstream stations and indicate recovery of the benthic community.

Metric values and 181 scores indicated no impact to the benthic community at monitoring locations downstream from Stations 214 and 215.

These results show only a short-term seasonal effect attributable to the discharge for Station 215 during the months of July and/or August. The shoreline area between Stations 214 and 215 likely experiences similar conditions and similar changes to the benthic community as the stations that bracket this area. Moreover, observations of 181 scores and metric values at Station 215 were similar to non-thermal stations and were higher than non-thermal Station 221.

Station 215 benthic community observations were not significantly different from the non-thermal stations.

Station 189, the next closest station downstream, is located 1.3 miles below the discharge canal. No impact to the benthic community was observed at Station 189. The benthos collection data show that the limit of measurable effect to the shoreline benthic community is farther upstream from Station 189 in the vicinity of Station 215. Relatively high metric values and 181 scores were observed at Stations 189, 216, and 217, with values at these locations comparable to or higher than those determined for the upstream, non-thermal stations. The benthos monitoring identified and confirmed that the thermal impact is confined to the western shoreline in the vicinity of the two stations closest to the end of P8APS discharge canal.

Field observations indicated that the amount of benthic area affected by the thermal plume is small in relation to the available benthic habitat area of Conowingo Pond. The areas of impact are confined to areas along the western shoreline directly downstream from the P8APS discharge. This area from the end of the discharge canal downstream to Station 189 comprises less than 19 acres of the total shallow shoreline habitat. Lower 181 scores and metric values indicate that the benthic macroinvertebrate community is affected in the near-field from the P8APS discharge canal downstream to Station 215, which encompasses approximately 12 acres of shallow shoreline habitat. The benthos survey data indicate that benthos impact is localized and temporary and occurs during July and August with recovery evident at Station 214 beginning in September.

An observable effect on the benthic community occurred during the July and August timeframe at Station 214 in 2010-2012. The observable impact at Station 215 occurred during July or August depending on the year of collection in 2010-2012. No measurable thermal impacts were detected in 2013 for either station (i.e., high 181 scores in July and August). The influence of the thermal plume resulted in fewer taxa being present in the July or August samples. During July and August the benthic community at Station 214 was dominated by a single taxon, Chironomidae, which comprised a majority of the organisms collected. This finding is consistent with studies that have shown several chironomid genera to be tolerant of elevated water temperatures (EPA 1978).

75

Final Report PBAPS Thermal Study Few studies have evaluated the chronic effects of elevated water temperatures on benthic communities or specific species and most did not account for acclimation temperature. The empirical evidence gained from this study is useful in understanding the changes to the benthic community related to elevated water temperatures. A more detailed discussion of the relation between water temperature and the benthic macroinvertebrate community is provided in the last part of Section 5.5.

Lower metric values and 181 scores in July and August resulted in significantly different benthic community at Station 214 as compared to most other non-thermal and thermal stations.

Removal of July and August collections from the analyses of monthly collections for all stations results in only one significantly different metric (Kruskal-Wallis, p > 0.05). The only significant difference was Trichoptera richness (Kruskal-Wallis, p = 0.008). Trichoptera richness was significantly different between Station 214 and Stations 217 and 208. This further illustrates the short-term seasonal nature of the thermal impact. Elevated water temperatures during other months did not result in detectable impact to the benthic community based on metric values and IBl score analyses.

The seasonal differences in metric values are likely related to establishment of SAV and life history patterns of certain benthic insects. Many of the Trichoptera and other taxa are obligates that depend on SAV for habitat and as a food source. This is quite apparent at several of the collection locations (e.g. Station 208) where the highest richness values where observed during the summer and fall. Station 214 did not show a similar seasonal trend. The elevated water temperatures during July and August likely limited the establishment of these specific taxa at Station 214 which led to lower overall richness values. Community composition as determined by 181 scores and metric values indicated that Station 214 benthos community is similar to other location during other months of the year. That is, richness, diversity and evenness are comparable during the spring and late fall to other non-thermal and thermally affected areas of the Pond. Interestingly, during 2013 with the lower ambient temperatures and higher River flows the 181 and metrics scores were much higher at Station 214 during July and August. The 181 score at Station 214 during July (50) was higher than all other stations during that month.

Although the PADEP multi-habitat protocol was not developed for use in reservoirs such as Conowingo Pond or designed to address benthic community impacts associated with elevated temperature, it did allow for a standardized approach to compare the collection stations. It is important to reiterate that the protocol methods employed in this study were utilized in the absence of a methodology specifically developed for impoundments and for assessing thermal impacts. The individual metrics and metric scoring criteria were not developed for assessing changes in benthos related to thermal effluents in an impounded waterbody. Thus, interpretation of the 181 scores is difficult and comparison of the 181 scores to the protocol threshold for determining water quality impact would not be appropriate.

Lastly, the shore zone benthos community was assessed and included as a component of this study at the request of PADEP. This shallow shore zone habitat is a small proportion of the entire available benthic habitat in the Pond. Most of the Pond benthic habitat is in open-water 76

Final Report PBAPS Thermal Study areas not along the shoreline. In terms of total organisms and biomass the open-water areas make up a much larger portion of the benthic community in the Pond.

Overall Conclusions 8enthic community effects resulting from the thermal plume are localized and temporary, with the area of impact being small in comparison to the amount of similar non-thermally impacted Conowingo Pond shoreline. The area from the P8APS discharge canal downstream to Station 215 represents approximately 12 acres of shallow shoreline habitat within Conowingo Pond from the vicinity of MRPSF to Conowingo Dam that is affected by the thermal plume. The assessment of shoreline habitat indicates a narrow band of shallow shoreline habitat within the area directly downstream from the P8APS discharge canal.

The simple benthic macroinvertebrate community present within the Pond can continue to complete necessary life-cycle stages regardless of the limited impact area and temporary impacts due to thermal discharge. This is evident in that benthic community persists in nearby shallow shoreline habitat and re-colonization of impacted areas occurs during September when water temperatures decrease and in subsequent months re-colonization continues. The benthic community present within the areas with lower 181 scores is similar to the other stations during the spring. This temporary local change to the benthic community does not affect the food resources of fish (see Section 5.6 Fish Condition).

8enthic macroinvertebrate collections were successfully completed from 2010-2013. The data indicate that:

  • Benthic community impacts resulting from the thermal plume are local and temporary and limited to a small proportion of the available shallow shoreline habitat within Conowingo Pond.
  • The composition and relative abundance of the benthic community were similar during all 4 years with variable numbers of cooling towers in operation.
  • The benthic community was characterized by similar diversity both within and outside of the thermal plume.
  • Temporary impact, in terms of lower 181 scores, was observed at Stations 214 and 215.

The lower 181 scores occurred after a sustained period of high water temperatures for a portion of July and August and, thereafter, recovery took place.

  • Observations over the course of the entire collection period indicated that no substantial reduction in community heterogeneity or trophic structure was observed at Stations 214 and 215.
  • There was no observed impact to the benthic community at the three thermally-influenced Stations (189, 216 and 217) that are farthest downstream from the discharge canal.
  • The benthic community was able to sustain itself through cyclical seasonal changes both within and outside of the thermal plume.
  • There is a balanced indigenous benthic community within Conowingo Pond.

77

Final Report PBAPS Thermal Study

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78

Final Report PBAPS Thermal Study

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79

Final Report PBAPS Thermal Study

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80

Final Report PBAPS Thermal Study

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81

Final Report PBAPS Thermal Study Table 5-12. Description of seine and benthos stations in Conowingo Pond (negative values indicate upstream from the discharge canal).

Distance From End Of Discharge Canal Station Description Meters Miles 189 Rock outcropping at north side of Michael's Run to 'McClellan's Rock'. 2,128 1.32 202 Southeast shore of Sicily Island. -6,331 -3.93 203 West shore of Big Chestnut Island -6,683 -4.15 208 Peach Bottom Beach. -2,449 -1.52 214 Beach at the mouth of Burkins Rwt 591 0.37 215 Campground boat launch' - about 250 m below the mouth of Burkins Run. 1,049 0.65 216 Below site 190, small cove at end of Line Bridge Road 3,919 2.44 217 2,000 m above the mouth of Conowingo Creek. 6,466 4.02 220 Coal Cabin boat launch. -4,410 -2.74 221 Fishing Creek confluence - northwest side of shoal -4,765 -2.96 Table 5-13. Description of trawl transects in Conowingo Pond. (negative values indicate upstream from the discharge canal).

Distance From End Of Discharge Canal Station Description Meters Miles Transect 2 321 Off PBAPS Unit 2. -1,824 -1.13 322 Mid-pond between Mt. Johnson Island and PBAPS. -2,035 -1.26 323 Below Mt Johnson Island -2,343 -1.46 Transect 3 331 McClellan's Rock 1,911 1.19 332 Mid-pond between McClellan's Rock and William's Tunnel 2,195 1.36 333 William'sTwmel 2,678 1.66 Transect 4 341 Broad Creek 5,022 3.12 342 Mid-pond off Broad Creek 4,483 2.79 343 Wildcat Tunnel 4,114 2.56 Transect 7 371 Burkins Run (Stonewall Point). 589 0.37 372 Mid-pond between Burkins Run and the former lchthyological Associates dock 1,013 0.63 373 lchthyological Associates Dock. 1,%5 1.22 Transect 8 381 Campground boat launch below Burkins Run. 1,042 0.65 382 500 m off west shore 1,322 0.82 383 500 m of East shore. 1,841 1.14 384 Chester County Water Intake. 2,456 1.53 82

Final Report PBAPS Thermal Study Table 5-14. Description of electrofishing stations in Conowingo Pond. (negative values indicate upstream from the discharge canal).

Distance From End Of Discharge Canal Station Description Meters Miles 161 Rock outcropping above Burkins Run to PBAPS discharge structure. 545 0.34 164 Southwest shoreline of Mt. Johnson Island -2,741 -1.70 165 East shoreline above Peters Creek. -2,159 -1.34 187 South of Rollins Point to fast cabin. -3,325 -2.07 189 Rock outcropping at north side ofMichaers Run to 'McClellan's Rock'. 2,128 1.32 190 First cabin below Michaels Run to mouth. 3,285 2.04 217 2,000 m above the mouth of Conowingo Creek. 6,466 4.02 Table 5-15. Descriptions of benthic macroinvertebrate community metrics.

Response

Metric Description to Impairment Richness The total number oftaxa. The PA DEP 95th percentile value is 31 taxa. decreases EPTindex A count of the number of mayfly (.Epherneroptera), stonefly (.flecoptera), decreases and caddisfly (Irichoptera) genera. The PA DEP 95th percentile value is 17 genera.

Modified Beck's 4 Index A weighted count oftaxa with Pollution Tolerance Values between 0 and 4. decreases Taxa with Toi. Values ofO or I are given 2 points. Taxa with Toi. Values between 2 and 4 are given I point. The PA DEP 95th percentile index value is 22.

Shannon Diversity (H) A measure of community balance in base e based on the distribution decreases of the taxa present (H = - Sum P, log P;). The PA DEP 95th percentile index value is 2.43.

Number of Mayfly Taxa A count of the number of genera in the order Ephemeroptera The PA DEP decreases 95th percentile value is 6 genera.

NumberofCaddisfly Taxa A count of the numberofgenera in the orderTrichoptera The PA DEP decreases 95th percentile value is 11 genera.

83

Final Report PBAPS Thermal Study Table 5-16 Habitat assessment scores for the 10 benthos stations.

Non-thermal Stations Thermal Stations Parameter 202 203 220 221 208 214 215 189 216 217 Epifaunal Substrate/Available 10 10 15 14 15 15 15 14 11 13 Cover Pool Substrate 5 10 16 15 15 15 15 12 11 14 Characterization Pool Variability 5 15 5 5 5 5 5 11 5 5 Channell Alteration 1 1 1 1 1 1 1 1 0 0 Sediment Deposition 5 5 15 5 15 10 15 18 14 16 Channel Flow Status 14 14 16 10 15 15 15 13 20 20 Condition of Banks 15 15 15 14 15 15 15 7 18 18 Bank Vegetative 5 5 10 15 15 18 15 10 12 16 Protection Riparian Vegetative 15 15 15 15 15 19 16 10 6 6 Zone Width Total Score 75 90 108 94 111 113 112 96 97 108 84

Final Report PBAPS Thermal Study Table 5-17. Percent composition of common benthic macroinvertebrates (>1%) collected from Conowingo Pond, July-October 2010.

Station Tax on 202 203 208 220 221 214 215 Oligochaeta 17.2 13.9 8.2 13.1 21.6 11.4 16.3 Acariformes 1.4 1.2 1.5 2.7 4.6 4.1 Bivalvia Corbicu/a 2.6 3.0 2.9 4.3 3.6 14.2 19.1 Gastropoda Ferrissia 7.9 4.0 Goniobasis 1.8 2.5 Gyrau/us 16.5 6.6 1.7 Helisoma 2.8 3.9 2.6 Physa 2.8 5.8 6.4 2.1 10.5 Odonata Enallagma 3.7 7.0 1.1 6.1 Amphipoda Gammarus 12.8 5.3 6.0 5.5 1.5 Ephemeroptera Ca en is 9.5 20.1 21.0 35.2 3.9 2.7 3.1 Callibaetis 2.9 2.4 Hexagenia 1.2 Stenacran 2.0 2.6 Trichoptera Oecetis 2.1 Orthotrichia 2.0 Diptera Chi ronomi dae 29.0 28.9 28.5 22.3 47.4 67.2 38.9 Coleoptera Stene/mis 1.4 Total Richness 12 11 11 9 9 5 9 Total EPT 2 2 4 1 2 1 2 85

Final Report PBAPS Thermal Study Table 5-18. Percent composition of common benthic macroinvertebrates (>1%) collected from Conowingo Pond, April-October 2011.

Station Taxon 202 203 208 220 221 214 215 216. 217" Nematoda 2.5 1.4 1.1 1.5 Ollgochaeta 17.0 29.9 15.9 24.6 31.9 22.4 21.6 32.7 16.5 Acariformes 14.7 3.6 2.2 3.8 Bi val via Corbicu/a 1.2 1.4 2.0 16.0 25.0 7.1 2.1 Pisidium 1.4 2.1 Gastropoda Goniobasis 10.0 Gyraulus 1.4 He/isoma 1.1 Physo 2.0 Odonata Enallagma 1.2 1.5 2.3 Amphipoda Gammarus 23.7 13.4 10.2 13.0 7.0 1.8 3.2 11.0 6.2 Ephemeroptera Caenis 3.5 2.3 9.8 3.2 2.2 1.7 9.7 20.1 Hexagenia 2.1 1.7 3.0 1.2 Stenacron 1.2 Trichoptera Orthatrichia 1.8 1.5 Diptera Psychoda 2.2 Chironomidae 30.4 27.6 36.9 46.9 44.1 52.0 39.9 28.6 42.6 Coleoptera Stene/mis 11.2 9.1 1.1 Total Richness 8 8 11 6 9 6 6 8 8 EPT Richness 1 1 2 2 0 2 2 3 2

  • collection occurred from June-October 86

Final Report PBAPS Thermal Study Table 5-19. Percent composition of common benthic macroinvertebrates (>1%) collected from Conowingo Pond, April-October 2012.

Station Taxon 202 203 208 220 221 214 215 189" 216 217 Nematoda 3.0 3.6 1.4 1.7 1.0 Oligochaeta 28.2 11.2 5.S 7.4 19.6 16.0 7.0 6.2 19.7 7.0 Acariformes 1.0 20.2 3.2 2.6 1.0 4.1 10.1 2.6 7.1 Bivalvia Corbiculo 7.5 12.1 2.9 2.6 3.0 10.5 14.7 22.1 3.0 2.2 Gastropoda Foss aria 9.1 4.3 Goniobosis 7.1 Gyroulus 2.8 4.2 13.1 Lymnaeidae 1.0 Physo 1.2 5.5 7.3 Pisidium 1.2 Odonata Argia 1.6 Enollogma 1.6 1.1 Amphipoda Crongonyx 2.2 1.0 Gammarus 24.0 19.7 9.0 12.7 2.6 7.5 4.8 15.8 5.7 Ephemeroptera Coen is 5.6 28.2 10.0 1.6 1.4 4.1 16.9 28.6 Moccoffertium 2.0 1.7 2.3 1.7 Stenacran 2.5 5.3 Hexogenia 3.7 5.7 Trichoptera Orthotrichio 1.2 Diptera Chironomidae 25.4 18.4 23.9 50.9 46.7 53.2 39.4 41.6 32.9 39.3 Coleoptera Stene/mis 1.9 14.7 2.6 Total Richness 9 10 8 8 11 7 12 7 9 8 EPT Richness 0 3 1 2 1 1 2 2 2 3

  • collections occurred from July-October 87

Final Report PBAPS Thermal Study Table 5-20. Percent composition of common benthic macroinvertebrates (>1%) collected from Conowingo Pond, April-October 2013.

Station Taxon 202 203 208 220 221 214 215 189 216 217 Oligochaeta 3.0 S.8 3.5 2.3 10.9 5.3 2.8 2.4 13.6 12.2 Acariformes 13.6 1.4 4.6 2.5 5.4 2.4 1.2 4.3 Turbe Ilaria Dugesio 1.2 Bivalvia Corbiculo 3.0 7.2 1.1 13.2 2.5 14.0 14.5 3.9 4.2 Gastropoda Ferrissio 1.6 2.3 Goniobosis 2.1 Gyrou/us 7.4 2.8 9.0 2.3 1.5 He/isomo 1.7 5.2 Physo 5.0 2.8 4.9 6.6 2.7 Odonata Enollogmo 1.0 Amphipoda Crongonyx 2.5 4.2 Gammorus 37.9 32.6 11.9 10.3 9.7 3.2 8.1 41.8 13.4 8.5 lsopoda Coecidoteo 2.4 4.3 Ephemeroptera Coenis 3.5 5.0 23.5 17.3 3.5 18.9 12.4 1.7 27.2 26.3 Stenocron 1.0 1.9 Col/iboetis 1.7 Hexagenia 2.9 Maccoffertium 1.2 Stenonemo 1.5 2.1 Trichoptera Hydroptilo 1.1 Oecetis 1.2 Orthotrichia 1.7 1.7 Lepidoptera Acentrio 1.8 Diptera Chironomidae 42.3 38.2 22.5 41.9 43.0 43.1 40.6 33.7 23.7 37.6 Coleoptera Dubirophio 1.1 Total Richness 7 7 12 8 11 9 10 10 10 7 EPT Richness 2 1 3 1 2 1 4 2 3 2 88

Final Report PBAPS Thermal Study Table 5-21. Benthic community composition at Station 214 during July and August, 2010-2012 and July and August 2013.

July 2010.20U July 2013 AU!!USt 2010.2012 August 2013 Percent Percent Percent Percent Taxon Number Comeosltion Number Comeositlon Number Comeositlon Number Comeosltion Acarlformes 3 0.5 11 5.6 1 0.2 15 6.8 Acentrla 1 0.5 Argla 1 0.5 Caenls 36 5.7 27 13.8 1 0.2 48 21.8 Callibaetis 1 0.2 1 0.5 Centroptilwn 1 0.5 Ceratopogon 1 0.5 Chlronomidae 409 65.1 65 33.3 436 80.0 101 45.9 Corbicula 112 17.8 1 0.5 13 2.4 34 15.5 Enallagma 4 0.6 1 0.5 5 0.9 2 0.9 Gammarus 32 16.4 Gomphidae 1 0.2 Goniobasis 6 3.1 Gyraulus 26 13.3 1 0.5 Hexagenia 2 1.0 Hydroptila 1 0.5 2 0.9 Nematoda 4 0.6 1 0.2 Oecetis 1 0.5 Orconectes 1 0.2 Ollgochaeta 56 8.9 1 0.5 80 14.7 Orthotric hia 1 0.5 Physa 2 0.3 9 4.6 6 1.1 12 5.5 Plsldlum 1 0.2 Stenacron 5 2.6 1 0.5 Stenonema 3 1.5 Triaenodes 2 1.0 Total Organisms 628 195 545 220 Total Richness 10 18 10 13 EPT Richness 1 7 2 6 Table 5-22. Summary metrics for benthos community, 2010-2013.

Metric 189 202 203 208 214 215 216 217 220 221 Total Organisms 1,881 4,257 4,543 5,035 4,700 4,780 3,650 3,870 4,987 4,4n Total Richness 41 52 55 55 49 54 45 44 65 56 Total EPT Richness 14 16 14 16 13 19 15 11 19 13 Percent Chironomidae 36.1 32.9 28.7 27.7 52.1 39.8 28.4 39.6 42.2 45.1 HBI 5.4 6.1 6.2 6.6 6.4 6.2 6.6 6.6 6.3 6.9

% Sensitive (TV 0-3) 0.3 0.5 1.2 1.1 0.2 0.8 2.6 1.5 0.9 0.2 Percent Oligochaeta 3.6 15.1 14.2 8.1 13.9 11.1 20.7 11.5 11.6 20.5 89

Final Report PBAPS Thermal Study Table 5-23. Mean and median 181 scores for stations within Conowingo Pond, 2010-2013.

IBI Score Number of Station Mean Median Samples 189 30.9 28.8h 11 202 30.0 29.5f 22 203 29.9 3lb 23 208 31.6 30.5e 25 214 20.5 18 8abcdefgh 25 215 29.5 28.38 25 216 32.7 34.5c1 19 217 31.0 30.9d 19 220 31.3 31.5a 25 221 23.7 23.61 25 IBI scores followed by the same letter were signficantly different (Kruskal-Wallis test, p<0.001)

Table 5-24. Median metric values for benthic macroinvertebrate collection locations in Conowingo Pond, 2010-2013.

Median Total Beck's Ephemeroptera Trichoptera EPT Total Shannon Number of Station Index Richness Richness Richness Richness Diversity Samples 189 4bdj 3d oh 3 11 1.3 11 202 31 2 1 4 12b l.6d 22 203 3k 2 ob 3 12e 1.5c 23 208 3Bl 2 2abcdfh 4ad 12' 1.6b 25 214 2abefhlk lb oaeg 1abce abcdef l. 2abcdef 8 25 215 3h 3c od 3 11 1.6e 25 acg 216 4 3ab oc 3e 12d l.r 19 217 3e 2 le 4d 12c 1.5 19 220 3f 2e lg 4bg 14ag 1.6f 25 221 2cd 1acde or 2dfg llg 1.2 25 Metric values followed by the same letter were significantly different (Kruskal-Wallis test, p s 0.001) 90

Final Report PBAPS Thermal Study Table 5-25. Mean total richness observed by month at each station, 2010-2013.

Station April May June July August September October st189 9.0 16.0 11.0 11.0 11.5 10.5 12.5 st217 10.5 11.5 10.3 13.3 13.7 14.7 12.7 st202 12.7 11.3 11.0 11.8 14.5 17.0 12.3 st203 12.0 7.7 10.3 11.3 15.3 15.3 13.3 st208 10.7 9.7 10.0 12.8 15.5 13.3 11.5 st214 10.3 9.0 10.0 9.8 7.8 9.3 8.0 st215 12.7 10.7 11.3 10.8 10.8 12.8 11.0 st216 13.5 11.5 9.7 11.7 14.7 12.0 14.0 st220 11.3 11.3 12.3 12.5 16.5 14.3 15.3 st221 8.0 10.3 10.7 8.8 13.0 12.5 13.5 Table 5-26. Mean EPT richness observed by month at each station, 2010-2013.

Station April May June July August September October st189 3.0 5.0 3.0 3.0 3.0 3.5 3.0 st217 3.0 2.0 2.0 4.0 4.0 5.3 3.7 st202 2.7 1.3 1.3 2.8 4.8 5.0 4.0 st203 2.5 0.7 0.7 2.8 3.8 5.5 3.0 st208 2.3 2.3 1.3 5.0 5.8 4.5 4.0 st214 0.3 1.0 2.3 2.5 2.0 2.0 2.0 st215 2.0 2.0 2.3 3.8 2.5 4.5 3.8 st216 4.5 1.5 2.0 4.0 5.0 3.7 3.0 st220 1.3 2.3 2.7 3.8 4.8 4.0 3.8 st221 0.7 1.0 1.3 1.5 3.3 2.8 2.8 Table 5-27. Mean Trichoptera richness observed by month at each station, 2010-2013.

Station April May June July August September October st189 0.0 2.0 1.0 1.0 0.0 1.0 0.0 st217 1.5 1.0 0.3 1.7 1.3 1.7 1.3 st202 0.3 0.7 0.3 1.3 1.8 1.5 1.0 st203 0.0 0.0 0.0 0.3 1.3 1.8 0.7 st208 1.3 1.3 0.7 2.5 2.8 1.8 2.3 st214 0.0 0.0 0.7 0.8 0.5 0.3 0.3 st215 0.3 0.0 0.3 0.8 1.0 1.5 0.5 st216 1.0 0.0 0.0 1.0 0.7 0.7 0.3

- -- ... - - st220 0.0 0.7 1.0 1.8 1.5 1.0 1.5 - - - --

st221 0.0 0.3 0.3 1.0 1.0 1.0 1.5 91

Final Report PBAPS Thermal Study Table 5-28. Mean Ephemeroptera richness observed by month at each station, 2010-2013.

Station April May June July August September October st189 3.0 3.0 1.0 2.0 3.0 2.5 3.0 st217 1.5 1.0 1.7 2.3 2.7 3.7 2.0 st202 2.0 0.7 1.0 1.5 3.0 3.5 3.0 st203 2.5 0.7 0.7 2.5 2.5 3.8 2.3 st208 1.0 1.0 0.7 2.5 3.0 2.8 1.8 st214 0.3 1.0 1.7 1.8 1.5 1.5 1.8 st215 1.7 2.0 2.0 2.8 1.5 3.0 3.3 st216 3.5 1.5 1.7 2.7 4.0 3.0 2.3 st220 1.3 1.7 1.7 2.0 3.3 3.0 2.0 st221 0.7 0.7 0.7 0.5 2.3 1.8 1.3 Table 5-29. Mean Shannon diversity values observed by month at each station, 2010-2013.

Station April May June July August September October st189 1.1 2.0 1.3 1.3 1.5 1.4 1.8 st217 1.5 1.4 1.5 1.6 1.4 1.8 1.3 st202 1.4 1.4 1.5 1.5 1.7 1.9 1.5 st203 1.6 1.1 1.3 1.4 1.8 1.9 1.8 st208 1.4 1.5 1.6 1.7 2.0 1.6 1.4 st214 1.2 1.2 1.3 1.2 0.9 1.2 1.1 st215 1.7 1.5 1.6 1.3 1.1 1.6 1.8 st216 1.6 1.4 1.5 1.8 1.9 1.7 1.6 st220 1.4 1.3 1.3 1.3 1.8 1.6 1.8 st221 1.1 1.4 1.1 1.1 1.4 1.6 1.7 Table 5-30. Mean Beck's Index values observed by month at each station, 2010-2013.

Station April May June July August September October st189 6.0 6.0 6.0 3.5 3.5 3.0 4.5 st217 3.5 3.5 2.0 3.7 3.3 4.7 3.0 st202 4.3 3.0 2.3 2.8 3.0 3.5 4.0 st203 5.0 1.7 2.0 3.3 3.8 3.5 3.3 st208 2.7 2.7 2.3 3.5 2.8 2.3 3.0 st214 2.7 2.0 2.0 1.5 1.8 2.8 1.8 st215 4.3 3.0 3.3 3.8 1.8 3.3 3.8 st216 4.5 2.5 3.3 5.0 4.7 4.0 4.0 st220 3.0 3.3 4.3 2.8 3.5 3.0 3.0 st221 2.3 3.0 3.7 1.8 3.0 2.0 2.5 92

Final Report PBAPS Thermal Study so 40 20 10 St203 St202 St221 St220 St208 St214 St215 St189 St216 St217 Figure 5-26. Box plot illustrating IBI Scores for each benthos station, 2010-2013. (boxes =

interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, and asterisk = outlier) 60 50 40 -~- -* ~

f!

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0 Figure 5-27. Box plot illustrating IBI scores for each year by benthos station, 2010-2013. (boxes

= interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box= highest and lowest values, and asterisk= outlier) 93

Final Report PBAPS Thermal Study 60 -

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0- I 11 11 I 11 I II I I 111 11 11 I 11 11 I I 11 11 111 I 11 11 Figure 5-28. Box plot illustrating 181 scores for each month by benthos station, 2010-2013. (boxes= interquartile range containing 50% of

=

the values, the line across the box median value, vertical lines extending from the box = highest and lowest values, and asterisk = outlier) 94

Final Report PBAPS Thermal Study 20.0 17.5 15.0

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7.5 5.0 st203 st202 st221 st220 st208 st214 st215 st189 st216 st217 Figure 5-29. Box plot illustrating total richness for each benthos station, 2010-2013. (boxes =

interquartile range containing 50% of the values, the line across the box = median value, vertical lines

extending from the box highest and lowest values, circle mean, and asterisk outlier) =

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interquartile range containing 50% of the values, the line across the box = median value, vertical lines

extending from the box highest and lowest values, circle mean, and asterisk outlier) =

95

Final Report PBAPS Thermal Study 6

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st203 st202 st221 st220 st208 st214 st215 st189 st216 st217 Figure 5-31. Box plot illustrating Ephemeroptera richness for each benthos station, 2010-2013.

(boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box= highest and lowest values, circle= mean, and asterisk =outlier) 4 3 * *

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st203 st202 st221 st220 st208 st214 st215 st189 st216 st217 Figure 5-32. Box plot illustrating Trichoptera richness for each benthos station, 2010-2013.

(boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) 96

Final Report PBAPS Thermal Study 7

6 5

0 0 0 0

2 1

0 st203 st202 st221 st220 st208 st214 st215 st189 st216 st217 Figure 5-33. Box plot illustrating Beck's Index values for each benthos station, 2010-2013.

(boxes interquartile range containing 50% of the values, the line across the box median value, vertical

=

lines extending from the box highest and lowest values, circle mean, and asterisk outlier) 2.5 2.0

~ 0

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  • 0.0 st203 st202 st221 st220 st208 st214 st215 st189 st216 st217 Figure 5-34. Box plot illustrating Shannon Diversity values for each benthos station, 2010-2013.

(boxes interquartile range containing 50% of the values, the line across the box median value, vertical

=

lines extending from the box highest and lowest values, circle mean, and asterisk outlier) 97

Final Report PBAPS Thermal Study year 40 D 2010 D 2011 D 2012

[* D 2013 30 f II

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St203 St202 St221 St220 St208 St214 St215 St189 St216 St217 Figure 5-35. Bar chart showing relation of mean 181 scores by year for each benthos station.

98

Final Report PBAPS Thermal Study 50 f

~ 30 iii 20 0

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J Figure 5-36. Box plot illustrating relation of monthly 181 scores for non-thermal (upstream) benthos stations and Stations 214 and 215, 2010-2013. (boxes= interquartile range containing 50% of the values, the line across the box= median value, vertical lines extending from the box = highest and lowest values, circle= mean, and asterisk = outlier) 99

Final Report PBAPS Thermal Study Benthos-Water Temperature Observations A total of five thermally influenced nearshore benthos stations were sampled during the course of the study (Figure 5-22). Four of these stations are located along the western shoreline at varying distances downstream from the P8APS discharge canal while the most-downstream station is about 4 miles downstream of P8APS on the eastern shoreline. The relation of benthic 181 scores and water temperature observed at the thermally influenced stations is important to understanding the potential impact to benthos in thermally influenced areas of the Pond where sampling did not occur. The temperature monitoring determined the thermal history at these locations at the River bottom where benthic organisms live (Section 3). Thus, the approach taken herein was to use empirical evidence from the current study to determine water temperatures that result in impact to benthos. A study-specific temperature metric was developed that can be used to evaluate and determine conditions that result in benthic impacts.

Unlike the fish-avoidance analysis on which a robust catalogue of scientific literature exists, few field studies have evaluated chronic effects of elevated temperatures on benthos and most did not account for acclimation temperature.

The following discussion regarding cumulative impact of elevated temperatures to benthic communities aids in elucidating the concept that temperature impacts to benthos are cumulative rather than instantaneous. The two thermally influenced benthos stations (214 and 215) closest to the P8APS discharge canal outfall experienced the highest water temperatures. For both stations a similar pattern of low 181 scores was observed during July and/or August. Figure 5-37 through Figure 5-40 show the relation of daily mean water temperature and 181 scores for Station 215; a similar relation was observed at Station 214 which is closer to P8APS. During the first 3 years of study, 181 scores were lower in July and/or August following periods with daily mean water temperature that exceeded 93°F (Figure 5-37 through Figure 5-40). Water temperature that exceeded 93°F for an extended period resulted in lower 181 scores.

Higher 181 scores and recovery of the benthic community were observed in subsequent months after water temperatures decreased. At both Stations 214 and 215 daily mean water temperatures exceeded 93°F during the course of study in July and/or August. Not surprisingly, the greatest number of days exceeding 93°F was observed at Station 214 (Table 5-31). Few days in 2013 at Stations 214 or 215 exceeded a daily mean water temperature of 93°F and both 181 scores and metric values did not indicate a thermal effect. Station 189 also experienced daily mean temperatures greater than 93°F during 201 O and 2011. However, benthos sampling was not initiated at this station until 2012. Daily mean temperature at Station 189 did not exceed 93°F during 2012 or 2013 and both metric values and 181 scores did not indicate thermal effect (Table 5-22 and Table 5-23). Daily mean water temperatures did not exceed 93°F at any of the other stations during the study (Table 5-31).

Interestingly, water temperature at the time of collection was not correlated to 181 scores. 181 score and water temperature pairs were analyzed with simple linear regression for Stations 214 and 215 (2010-2013) with no correlation between pairs (R 2 ~0.03, p >0.1 ). Figure 5-41 illustrates the relation of mean water temperature and 181 score at Station 215 for all months 100

Final Report PBAPS Thermal Study and years combined. 181 scores were variable across month and years with generally higher scores observed in 2013 for most months and highly variable 181 scores observed at the highest water temperatures. A similar result was observed for Station 214. These results support the conclusion that the duration of elevated water temperatures prior to collection was crucial in causing impacts to the benthic community as reflected in the corresponding low 181 scores.

The results observed in 2013 indicate that 5 or 7 days of water temperatures greater than a daily average of 93°F did not result in a benthic effect for Stations 214 and 215, respectively.

The actual number of days greater than the threshold temperature of 93°F that would result in benthos impact cannot be determined exactly from the currently available data. However, it is probable that greater than 7 days of elevated water temperatures are required . In 2010-2012 daily mean temperature at Station 215 was greater than 93°F from 21 to 25 days with a corresponding drop in 181 score after the period of elevated temperature for each year. Based on the available data between 7 and 21 days of elevated water temperatures greater than daily mean of 93°F will result in benthic impacts.

A benthic model was developed based on the empirical results discussed above in order to evaluate potential benthic impact of high discharge temperature after implementation of EPU.

The constraints of the Benthic Impact Model require a determination of potential impact based on instantaneous rather than mean water temperature. Thus the model was used to determine areas of the near-shore River bottom that experienced instantaneous water temperatures greater than 94°F for both the typical and extreme case. The instantaneous value of 94 °F was selected to be used as a conservative analogue to the 93°F temperature-ISi score metric.

Using the instantaneous value of 94°F rather than daily mean of 93°F is more conservative and results in larger areas of potential benthic impact. As indicated in Table 5-32 the conservative instantaneous approach spatially encompasses a greater number of benthos sample stations and thus would predict a larger area of potential benthos impact than was actually observed during this study. Evaluation of potential impacts using the Benthic Impact Model are discussed and illustrated in Section 7.

101

Final Report PBAPS Thermal Study 100 r so Y.

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10 s 0 0 4/1 4/26 S/21 6/lS 7/10 8/4 8/29 9/23 10/18 Figure 5-37. Relation of 181 score and water temperature for Station 215 in 2010.

100 1 so

-~90 I!! 80 45 40

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E 10 - .-r"'- IBI Score 5 0 0 4/1 5/1 6/1 7/1 8/1 9/1 10/1 11/1 Figure 5-38. Relation of 181 score and water temperature for Station 215 in 2011.

102

Final Report PBAPS Thermal Study 100 50 u.

QI 90 80 45 40

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100 50 90 45 I.&.

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103

Final Report PBAPS Thermal Study Table 5-31. Number of days each year with daily mean water temperature >93°F for all stations, April 1 to October 31.

Station 2010a 2011 2012 2013 220 0 0 0 0 PBAPS Intake 0 0 0 0 208 0 0 0 0 214 28 36 39 7 215 25 25 21 5 189 4 11 0 0 190 0 0 0 0 216 0 0 0 0 217 0 0 0 0 aMonitoring did not begin until July 28 Table 5-32. Number of days each year with instantaneous maximum water temperature >94 °F for all stations, April 1 to October 31.

Station 2010a 2011 2012 2013 220 0 0 0 0 PBAPS Intake 0 0 0 0 208 0 0 0 0 214 32 39 43 8 215 28 30 36 8 189 4 14 5 1 190 1 8 1 0 216 0 7 2 0 217 0 0 1 1 aMonitoring did not begin until July 28 104

Final Report PBAPS Thermal Study Figure 5-41. Relation of daily mean water temperature and 181 score for Station 215, August-October, 2010 and April-October, 2011-2013.

Station 215 50 year Odober

  • 2010
  • Sep~ber
  • 2011 August July 2012 April 40 Sept;'ber ..... 2013 cu Odober Odober June July a..

0 30 * ~ July

~ April

  • September June Odober May i April
  • May September June
  • ,,st 20 *

,st 10 R2=0.03, p = 0.43 August 60 70 80 90 100 Mean Water Teq>erature ( 0 F) 105

Final Report PBAPS Thermal Study

5. 6 Fish Community The spatial and temporal distribution of fish was evaluated by monthly sampling at both thermally influenced and non-thermally influenced locations in July through October 2010 and April through October 2011-2013. In addition, winter electrofishing events were completed in January, February, or March 2011-2013. The relative abundance of all fish was determined by standardizing the number of individuals of each species collected per unit of collection effort for each of the three sampling gear types. The methods employed in the fisheries study are briefly described below, followed by discussion of the sampling results and analyses for the entire 4-year study. The results from 2010, 2011, and 2012 were reported in three interim annual reports (Normandeau Associates and ERM 2011, 2012 and 2013a).

Methods Seining was conducted at seven shoreline stations (Table 5-12; Figure 5-22) located in areas thermally affected by the plume and in unaffected areas upstream of PBAPS and on the east shore of the Pond. Stations 214 and 215 are considerably influenced by the PBAPS thermal plume as determined by observations of water temperature and velocity of the thermal discharge plume. Data recorded at each station for each collection included weather, date, time, Secchi disc transparency, air and surface water temperatures, dissolved oxygen, and estimated water depth. Appendix 11.2 provides water chemistry data collected during the field collections.

A 10 x 4-ft straight seine with %-inch mesh was used. The seine was deployed and moved parallel to shore for a short distance, then moved into shore to trap fish; this effort constituted one seine haul. Since size and habitat of seine stations varied, an effort was made to collect a representative sample based on complete coverage of all available habitats, limiting the number of hauls at each station to five. All specimens were identified, counted, and released near the capture site. Specimens that were too small to accurately identify to species in the field were only identified to genus.

E/ectrofishing Electrofishing was conducted at night at seven stations located along the shores of Conowingo Pond (Figure 5-23; Table 5-14). Stations 161, 189, 190, and 217 are located sequentially below PBAPS and are influenced by the thermal discharge from PBAPS, with Station 161 being most thermally influenced and Station 217 being the least influenced. The electrofishing system consisted of a Smith-Root WP-158 variable voltage pulsator, powered by a 3.5-kW generator, and mounted in an 18-ft aluminum boat equipped with a bow-mounted T-boom cathode array and flood lights. Fishes were collected using pulsed direct current to minimize fish injury. Data recorded for each collection included weather, date, time (start and end), air and surface water temperatures, dissolved oxygen, conductivity, voltage, and amperage. Appendix 11.2 provides water chemistry data collected during the field collections.

Sampling at each location consisted of a 30-minute run and was typically completed in one pass through the sampling location. The electrofishing boat was maneuvered slowly through the site, 106

Final Report PBAPS Thermal Study as close to shore as possible. Stunned fish were netted at the bow and placed in a live well.

Large stunned specimens of Common Carp and Quillback were not netted, but were counted by the netting crew and recorded. At the end of 30 minutes, the boat was returned to the center of the station, and the catch processed. Each fish was identified to species, measured to the nearest millimeter (mm) total length (TL), weighed to the nearest gram, and released. When a large number (>50) of a single species was collected, a subsample of 50 specimens was measured into 1O mm TL intervals, batch weighed, and an exact count was made of the remainder and released.

Trawl Bottom trawl sampling was conducted at five transects (2, 3, 4, 7, and 8) as depicted in Figure 5-24. Each transect was composed of an east shore, mid-pond, and west shore sampling station, except Transect 8 which had two mid-pond stations due to the greater width of the river at this location. Transect Stations 331, 371, 381, and 382 are within the area influenced by PBAPS thermal discharge, but substantial temperature increases do not extend to the bottom of the Pond. Trawl sampling was not performed in 2013.

Table 5-13 provides a description of the location of the trawl stations. Data recorded for each trawl sample include weather, date, time (start and end), Secchi disc transparency, air temperature, and water depth, along with water temperature and dissolved oxygen at the surface, mid-depth, and bottom.

Samples were collected using a 16-ft semi-balloon otter (bottom) trawl with %-inch mesh liner in the cod end. The trawl was deployed off the stern of the boat and hauled for 10 minutes in an upstream direction. A minimum of 7 minutes was required for the haul to be considered valid.

After the required sampling duration the trawl was retrieved, the boat was returned to the center of the station, and the catch was removed from the net and processed. All specimens in each collection were identified, measured to the nearest mm TL, and released. When a large number

(>50) of a single species was collected, a subsample of 50 specimens was measured into 1O mm TL intervals and an exact count was made of the remainder and released.

Catch Overview This section provides a general summary of the fish catch information produced by the seine, electrofishing and trawl sampling conducted in 2010 through 2013. Table 5-33 provides a list of common and scientific names of fish species observed in Conowingo Pond during the course of this study. This sampling program continued the fish community monitoring that has been performed periodically in Conowingo Pond relative to PBAPS for over 40 years.

The three sampling methods used in this study were deployed in somewhat different habitats and tend to target certain species and sizes of fish, but together they provide a comprehensive understanding of the fish community in the Pond. For example, trawling collects fish on the bottom of the Pond in offshore, generally deep areas, whereas seining and electrofishing are performed at shallow shore-zone sampling stations. In addition, seining collects predominantly 107

Final Report PBAPS Thermal Study small-bodied fish, often the young of species that attain a large size as adults. Electrofishing is effective for both large and small fish.

Fisheries data from each gear type are expressed as catch (numbers of individuals) per unit effort (CPUE) by station; monthly catches for each gear are expressed as number of individuals for all stations combined . Seine CPUE is expressed as number of each species per collection.

The trawl CPUE data are presented as number of each species per 10-minute haul, with electrofishing CPUE expressed as the number of fish captured per 30 minutes of sampling.

Over 90,000 specimens of more than 50 species were collected in this study at sampling stations in Conowingo Pond (Table 5-34 through Table 5-37). The fish assemblage was comprised of various feeding guilds including piscivores, a filter feeder, omnivores, insectivores, generalists, and invertivores. A list of the trophic designation for common species and RIS collected in Conowingo Pond is provided in Table 5-38. Presence of these various groups and their common occurrence (relatively high abundance) in the Pond indicates multiple trophic levels within the fish community and multiple levels of the food chain that includes forage species and predator species. Various representative trophic groups were observed at both thermally and non-thermally affected stations.

Inter-annual and monthly variation in the relative abundance of the various species as collected by the three sampling methods were often substantial due to variability in spawning success and species-specific preference for and avoidance of the habitats sampled. Gizzard Shad was the most numerous species collected by the three sampling methods combined in 2010 and 2011, Comely Shiner (not an RIS) was most abundant in 2012, and Bluegill was most numerous in 2013. Among the RIS, Spotfin Shiner, Bluegill, and Channel Catfish often ranked among the five most abundant fishes and these individual species usually comprised at least 5% of the combined catch each year. Other RIS such as White Sucker, Largemouth Bass, Chesapeake Logperch, and Walleye were collected in relatively low numbers each year. White Crappie was the least numerous RIS in all years.

Annual summaries of the seine data, with the results grouped by thermally affected and non-thermally affected stations, are presented in Table 5-40, Table 5-43, Table 5-46, and Table 5-49. Sample Stations 214 and 215 were categorized as thermally influenced while the remaining five seine stations were judged to be non-thermally affected, as they were located upstream of PBAPS or on the east shore opposite PBAPS. Spotfin Shiner was the most numerous species taken by seine each year except in 2013 when Bluntnose Minnow was slightly more abundant. Other numerous species in one or more years included Bluntnose Minnow, Banded Killifish, Bluegill, Spottail Shiner, Gizzard Shad, and Comely Shiner.

Evaluation of the annual summaries of catches at the two thermally affected as compared to the five non-thermally affected stations is hampered by the disparity of numbers of stations in each group. However, Table 5-40, Table 5-43, Table 5-46, and Table 5-49 provide an annual comparison between thermal and non-thermally affected station based on average CPUE.

In 2010, July and August accounted for half of the months sampled. However, overall the data show similar fish communities at each station, although the fewest number of species was collected at both of the thermally affected stations in 2010 and one of them (Station 215) in 108

Final Report PBAPS Thermal Study 2011, 2012, and 2013. As will be discussed in a following section of this report, the decreased catches at high plume temperatures in July and/or August are an indication that fish are temporarily avoiding the high temperature water. Otherwise, the data show no discernible pattern in number of fish per collection and relative abundance by species relative to thermal influence. That is, collections during the other months do not indicate avoidance at Stations 214 or 215; rather, the community composition and relative abundance are comparable to the other stations outside of the plume.

In the electrofishing catch, Gizzard Shad was by far the most numerous species collected in 201 O and 2011, but in 2012 it was overshadowed by high numbers of Comely Shiner and Bluegill (Table 5-39, Table 5-42, and Table 5-45). In 2013, Gizzard Shad and Bluegill were collected in similarly high numbers. Other common species in the electrofishing catch in one or more years included Channel Catfish, Spotfin Shiner, Bluntnose Minnow, and Smallmouth Bass.

A similar number of species was collected at the thermally affected ( 161, 189 and 190) and non-thermally affected stations (164, 165, and 187) in each year of the study. Overall, due to the similarities in the annual summary data, it is apparent that a SIC is being maintained at the thermally affected and unaffected stations.

As with the other gear types, the trawl data collected in 201 O - 2012 are characterized by high variability between stations and years, with no consistent indication of a thermal impact to the BIC at the thermally affected locations (Table 5-41, Table 5-44, and Table 5-47). Channel Catfish was the most numerous species in 2010 and 2011 and at most sample stations. In 2012, Gizzard Shad was most numerous. Other species taken in relatively high numbers in one or more years include Bluegill, Tessellated Darter, Common Carp, and Spottail Shiner. Spotfin Shiner was uncommon in the bottom trawl collections. Other RIS, such as Walleye, Chesapeake Logperch, Smallmouth Bass and Largemouth Bass, were infrequently collected.

The trawl surveys indicated no impact to the fish community from the PBAPS thermal discharge at the thermally affected locations. Fish abundance and species composition observed at the collection stations closest to the thermal discharge were similar to those observed upstream and farther downstream from the thermal discharge. Trawl collections focus on collecting fishes inhabiting the bottom or near-bottom strata of the water column. The water temperature profile for the PBAPS thermal plume shows that water temperatures are highest at the surface of the water column and that a gradient exists where temperatures decrease as a function of depth in the water column. The primary areas of concern for fish relative to elevated water temperatures are shallow water areas and surface waters in the immediate vicinity of the discharge. Trawl collections do not collect fish from shallow water areas or surface waters. Trawl sampling was suspended, upon consultation with PADEP, after the 2012 field season because the thermal plume is predominantly a surface phenomenon and the temperature data collected during field sampling did not show a substantial temperature rise at the bottom of the Pond.

This high-level overview of the multi-year fish sampling data shows that:

  • The fish community has the ability to sustain itself through cyclical seasonal changes,
  • Numerous prey species are present and relatively abundant in the fish community, 109

Final Report PBAPS Thermal Study

  • Pollution- or heat-tolerant species do not dominate the fish community,
  • No benefit was observed in terms of overall fish community composition or relative abundance from reduction in temperature resulting from cooling tower operation, and

110

Final Report PBAPS Thermal Study Table 5-33. List of common and scientific names of fishes collected in Conowingo Pond, 2010-2013.

Clupeidae Herrings Osmeridae Smelts Alosa pseudoharengus Alewife Osmerus mordax Rainbow smelt Alosa sapidissima American shad Dorosoma cepedianum Gizzard shad Belonidae Needle fishes Strongylura marina Atlantic needlefish Salmonidae Trouts Sa/mo trutta Brown trout Poeclliidae Live bearers Gambusia holbrooki Eastern mosquilofish Cyprlnldae Carps and minnows Campostoma anomalum Central stoneroller Cyprinodontidae Killifishes C/inostomus funduloides Rosyside dace Fundulus diaphanus Banded killifJSh Cyprinella spiloptera Spotfm shiner Cyprinus carpio Common carp Percicllfhyidae Temperate basses Ctenopharyngodon idella Grass carp A4orone americana White perch Exoglossum maxi/lingua Cutlips minnow Morone saxati/is Striped bass Luxilus cornutus Common shiner Nocomis micropogon River chub Centrarchidae Sunfishes Notemigonus crysoleucas Golden shiner Ambloplites rupestris Rock bass Notropis amoenus Comely shiner Lepomis auritus Redbreast sunfish Notropis hudsonius Spottail shiner Lepomis cyanellus Green sunfish Notropis procne Swallowtail shiner Lepomis gibbosus Pumpkinseed Notropis rube I/us Rosyface shiner Lepomis macrochirus Bluegill Notropis volucellus Mimic shiner Micropterus dolomieu Smalhnouth bass Pimephales notatus Bluntnose minnow Micropterus sa/moides Largemouth bass Rhinichthys atratulus Blacknose dace Pomoxis annularis White crappie Semotilus atromaculatus Creek chub Pomoxis nigromaculatus Black crappie Semotilus corpora/is FallfJSh Esocidae Pikes Catostomldae Suckers Esox masquinongy Muskellunge Carpiodes cyprinus Quillback Catostomus comrnersoni White sucker Percidae Perches Hypentelium nigricans Northern hog sucker Etheostoma blennioides Greenside darter Moxostoma macrolepidotum Shorthead redhorse Etheostoma olmstedi Tessellated darter Etheostoma zonale Banded darter lctaluridae Bullhead catfishes Perea flavescens Yellow perch lctalurus punctatus Channel catfish Percina bimaculata Chesapeake logperch Pylodictis olivaris Flathead catfish Percina peltata Shield darter Stizostedion vitreum Walleye 111

Final Report PBAPS Thermal Study Table 5-34. Number and percent (%) composition of fishes collected by all gear types in Conowingo Pond, July through October 2010. Species in bold are designated as RIS for this study.

July August September October Total O/o GiZ1.ard shad 2,867 538 2,422 78 5,905 47.4 Spotfin shiner 345 223 246 247 1,061 8.5 Common carp 19 12 34 16 81 0.7 Golden shiner 6 3 3 5 17 0.1 Comely shiner 36 22 27 70 155 1.2 Spottail shiner 20 41 25 14 100 0.8 Swallowtail shiner 2 3

  • 6 +

Bluntnose minnow 20 33 37 41 131 1.1 Creek chub * * * +

Fallftsh * * * +

Quillback 9 5 16 0.1 White sucker s *

  • 1 6 +

Northern hogsucker 5 2 6 14 0.1 Shorthead redhorse 4

  • 8 29 41 0.3 Channel catfish 662 600 237 718 2,217 17.8 Flathead catftsh 5 4 9 3 21 0.2 Banded killiftsh 3 39 142 185 1.5 White perch *
  • 4 5 +

Rock bass 44 26 16 68 154 1.2 Redbreast sunftsh * * * +

Green sunftsh 32 122 222 221 597 4.8 Pumpkinseed *

  • 2 +

Bluegill 105 215 480 320 1,120 9.0 Smallmouth bass so 16 40 66 172 1.4 Largemouth bass 4 3 8 46 61 o.s White crappie 1 *

  • 1 2 +

Black crappie * *

  • 2 2 +

Greenside darter

  • 3 10
  • 13 0.1 Tessellated darter 23 48 31 95 197 1.6 Banded darter
  • 2 2 5 +

Yellow perch * * * +

Chesapeake logperch 21 20 11 25 77 0.6 Shield darter

  • 3 5 9 0.1 Walleye 2 3 3 71 79 0.6 Overall 4,290 1,945 3,922 2,298 12,455 99.7 Number of species 27 25 27 28 34 Diversity 1.23 1.95 1.47 2.35 1.83

+Less than 0.05%.

112

Final Report PBAPS Thermal Study Table 5-35. Number and percent (%) composition of fishes collected by all gear types in Conowingo Pond, February and April through October 2011.

Feb" Apr May Jun Jul Aug Sep Oct Total  %

Alewife * * * * * * * +

American shad * * * * * * +

GiZl.Brd shad 57 372 341 34 2,251 7,027 95 88 10,265 40.0 Spotlin shiner 5 130 74 311 750 225 202 245 1,942 7.6 Common carp 8 37 36 39 39 30 26 24 239 0.9 Common shiner 2 * *

  • 4 *
  • 7 +

River chub * * * * * * * +

Golden shiner

  • 2 I 2 6 2 15 0.1 Comely shiner 126 71 31 3 17 142 121 1,945 2,456 9.6 Spottail shiner 3 33 5 14 179 173 314 310 1,031 4.0 Swallowtail shiner
  • 2 * * * *
  • 3 +

Mimic shiner 17 2 *

  • 5
  • 25 0.1 Bluntnose minnow 83 36 38 36 49 188 66 49 545 2.1 Creek chub 2 * * * *
  • 1 3 +

Fallfish 13 I *

  • 14 3 3 35 0.1 Quillback
  • 3 3 63 5 11
  • 86 0.3 White sucker
  • 3 2 * *
  • 7 +

Northern hogsucker * *

  • I 12 JO 3 27 0.1 Shorthead redhorse 6 2 8 13 25 25 24 104 0.4 Channel catfish 2 361 166 552 719 2,752 393 270 5,215 20.3 Flathead catfJSh I 4 12 6 II 2 3 39 0.2 Rainbow smelt * * * * * * * +

Eastern mosquitofJSh * * * * * * * +

Banded killifJSh

  • 7 23 18 7 I 4 28 88 0.3 White perch * * *
  • 4 7 9 15 35 0.1 Striped bass * * * * *
  • I +

Hybril Striped bass * * * *

  • 4 5 9 +

Rock bass 2 34 38 92 25 29 50 83 353 1.4 Redbreast sunf15h I

  • 2 I 2 8 +

Green sunfJSh 4 9 39 77 32 586 84 79 910 3.5 Pumpkinseed *

  • 3 I 4 II +

Bluegill 30 16 36 142 163 449 258 301 1,395 5.4 Smallmouth bass 8 21 30 43 60 43 91 85 381 1.5 Largemouth bass 18 3 2 4 19 9 29 24 108 0.4 White crappie I * *

  • 8 7 18 0.1 Black crappie 2 * * * * *
  • 3 +

Greens ile darter * * *

  • 5 *
  • 6 +

Tessellated darter 68 3 2 9 6 26 116 0.5 Yellow perch

  • 3
  • 2 2 5 14 0.1 Chesapeake logperch *
  • 2 7 6 39 6 5 65 0.3 Shield darter
  • 9 I II *
  • 23 0.1 Walleye 35 9 5 2 21 23 97 0.4 Overall 389 1,254 899 1,413 4,429 11,802 1,850 3,654 25,690 99.8 Number of species 24 28 26 25 28 29 33 28 41 Diversity 2.11 2.08 2.15 1.98 1.60 1.32 2.46 1.82 1.99
  • Sampling in February was limited to electrofJShing only.

+ Less than 0.05%.

113

Final Report PBAPS Thermal Study Table 5-36. Number and percent (%) composition of fishes collected by all gear types in Conowingo Pond, January, February and April through October 2012.

Jan* Feb* Apr May Jun Jul Aug Sep Oct Total  %

Gizzanls had 9 10 561 29 47 2,411 3,313 847 1,161 8,388 24.4 Rosyside dace 8 8 +

Spotfin shiner 3 92 213 121 2S9 246 67 118 1,120 3.3 Common carp 4 21 40 15 22 15 37 36 27 217 0.6 Cutplis minnow

  • I +

Common shiner +

River chub

  • 2 2 +

Golden shiner

  • 18 7 17 2 46 0.1 Comely shiner 1,825 3,905 709 97 20 206 154 2,309 148 9,373 27.3 Spottail shiner J02 42 114 58 33 81 89 156 35 7JO 2.1 Swallowtail shiner 2
  • 4 +

Rosyface shiner

  • I +

Mimic shiner

  • 2 3 +

Bluntnose minnow 19 26 93 65 2S IS 97 61 41 442 1.3 Creek chub 3 16 20 0. 1 Fallf15h

  • 2 7 3 14 +

Quillback 2

  • 7 2 2 2 3 18 0. 1 White sucker *
  • 5 II 8 I 2 1 3 31 0.1 Northern hogsucker I 6 15 7 2 32 0.1 Shorthead redhorse I 4 3 15 21 31 40 70 62 247 0.7 Channel catfish 8 2 263 197 233 591 661 414 380 2,749 8.0 Flathead catflSh 3 8 6 12 4 JO 44 0.1 Tiger Muskellunge * +

Atlantic needleflSh *

  • 5 5 +

Banded killif1Sh 16 5

  • 20 24 65 0.2 White perch 28 2 9 22 62 0.2 Striped bass * +

Hybrid Striped bass 2 4

  • 23 30 0.1 Rock bass 7 8 42 81 22 34 23 45 41 303 0.9 Redbreast sunflSh
  • 2 4 I
  • 2 II +

Green sunf1Sh 5 17 41 29 48 79 676 171 220 1,286 3.7 Pwnpkinseed 5 2 JO +

Bluegill 19 20 150 189 117 196 3847 2881 721 8,140 23.7 Smallmouth bass 10 12 36 S7 44 S4 32 79 63 387 I.I Largemouth bass 13 12 21 II 7 6 4 SI 23 148 0.4 White crappie

  • 3 * * *
  • s 3 12 +

Black crappie 2 2 2 7 +

Greenside darter *

  • 2 3 +

Tessellated darter 2 14 15 22 13 49 23 52 190 0.6 Yellow perch 6 3 I 4 8 23 0.1 Chesapeake logperch *

  • 6 9 6 IS 19 13 12 80 0.2 Walleye 7 4 6 I 2 3 4 7 87 121 0.4 Overall 2,041 4,089 2,219 1,125 794 4,074 9,342 7,295 3,293 34,356 99.8 N wnber of species 17 18 24 28 27 26 30 29 30 40 Diversity 0.79 0'42 2.96 3.69 3.74 2.22 2.21 2.42 3.07 2.82
  • Sampling in January and February was limited to electroflShing only.

+ Less than 0.05%.

114

Final Report PBAPS Thermal Study Table 5-37. Number and percent(%) composition of fishes collected by boat electrofishing and seining in Conowingo Pond, January, March and April through October 2013.

Jan* Mar* Apr May Jun Jul Aug Sep Oct Total  %

Gizzard shad 83 125 1049 1369 24 63 138 140 55 3046 16.6 Spotfin shiner 15 I 56 284 404 275 136 107 112 1390 7.6 Central stoneroller * * *

  • I 4 *
  • 6 +

Grass carp * * * * * *

  • I +

Common carp

  • 33 28 5 5 3 10 6 17 107 0.6 Golden shiner *
  • 8
  • 8 20 0.1 Comely shiner 200 693 219 88 37 33 145 373 165 1953 10.6 Common shiner * * *
  • I * * *
  • 1 +

Spottail shiner 95 58 89 20 38 69 176 132 69 746 4.1 Swallowtail shiner * * * *

  • 2
  • 4 +

Mimic shiner

  • 2 * * * * *
  • 2 +

Bluntnose minnow 346 39 234 176 141 103 127 204 118 1488 8.1 Blacknose dace * * * *

  • I * * +

Creek chub

  • 8 3 * * * *
  • 12 0.1 Fallfish *
  • 4 * * * * *
  • 4 +

Quillback * *

  • 22 2 *
  • 26 0.1 White sucker * * *
  • 69 2 30
  • 102 0.6 Northern hogsucker * *
  • 2 4 4 *
  • IO 0.1 Shorthead redhorse 2 8 27 29 57 30 44 65 38 300 1.6 Channel catfish 14 83 99 104 174 205 168 83 931 5.1 Flathead catfish *
  • 2 3 7 2 14 11 I 40 0.2 Muskellunge * * * * * * *
  • I +

Brown trout I * * * * *

  • 2 +

Banded killifish 5 6 20 113 57 3 20 43 433 700 3.8 White perch *

  • 4 17
  • 4 22 49 0.3 Hybrid Striped bass
  • 4 * * * * *
  • 5 +

Rock bass 3 2 89 59 30 23 22 38 151 417 2.3 Redbreast sunfish I 2 4

  • 3 2 13 0.1 Green sunfish 83 15 142 203 157 135 243 362 338 1678 9.1 Pumpkinseed * *
  • 2 2
  • 6 8 19 0.1 Bluegill 210 60 160 371 218 158 334 781 954 3246 17.7 Smallmouth bass 18 5 55 71 157 217 125 171 305 1124 6.1 Largemouth bass 29 20 15 8 9 9 27 12 20 149 0.8 White crappie 5 *
  • 2 4 5 5 22 0.1 Black crappie 5 2 * *
  • I *
  • 9 +

Greenside darter 3 * * *

  • 2 2 15 5 27 0.1 Tessellated darter 22
  • II 22 5 8 5 15 37 103 0.6 Chesapeake logperch 2
  • 2 3 9 37 78 153 53 337 1.8 Shield darter * * *
  • 2 7 17 12 39 0.2 Walleye JO 13 12 2 2 22 8 39 109 0.6 Overall 1140 1105 2346 2969 1580 1369 1944 2853 3075 18381 99.8 Number of species 22 23 24 25 29 29 28 28 29 41 Diversity 2.96 2.16 2.97 2.80 3.54 3.47 3.80 3.48 3.42 3.70
  • Sampling in January and March was limited to electrofJShing only.

+ Less than 0.05%.

115

Final Report PBAPS Thermal Study Table 5-38. Trophic designation of common species and RIS collected in Conowingo Pond, 2010-2013. Trophic designation assigned based on Barbour et al. 1999 and Roth et al. 2000.

Species Trophic Designation Banded darter IS Banded killifish IV Black crappie GE Bluegill IV Bluntnose minnow OM Channel catfish OM Chesapeake logperch IS Comely shiner IV Common carp OM Common shiner IV Creek chub GE Flathead catfish p Gizzard shad FF Golden shiner OM Green sunfish GE Greenside darter IS Largemouth bass p Northern hog sucker IV Pumpkinseed IV Quill back OM Rock bass GE Shield darter IS Shorthead redhorse OM Smallmouth bass p Spotfin shiner IV Spottail shiner OM Swallowtail shiner IV Tessellated darter IV Walleye p White crappie p White perch IV White sucker OM Yellow perch GE P=Piscivore H=Herbivore OM=Omnivore IS=lnsectivore (including specialized insectivores)

FF=Filter feeder GE=Generalist feeder IV=lnvertivore 116

Final Report PBAPS Thermal Study Table 5-39. Summary of fisheries data collected by boat electrofisher, July through October 2010.

Non-thennaUv Affected Total Nwnber/ Tiiermsllv Affected Total Nwnber/

Taxon 164 165 187 Nwnber Collection 161 189 190 Nwnber Collection Total  %

Gizzard shad 721 48 79 848 70.7 2,333 2,123 503 4,959 413.3 5,807 67.5°/o Spotfln shiner 62 21 44 127 10.6 14 29 JO 73 6.1 200 2.3%

COl1Il10ll carp 13 9 17 39 3.3 7 I 5 13 I.I 52 0.6%

Golden shiner Comely shiner Spottail shiier 14 9

24 12 I

24 16 I

62 37

0. 1 5.2
3. 1 2

12 3

3 13 32 I

16 44 6

1.3 3.7 0.5 17 106 43 0.2%

1.2%

0.5%

Bluntnose minnow 7 10 12 29 2.4 J 3 5 II 0.9 40 0.5%

Quillbock

\"11ite sucker NCJ'them hog sucker I

I 3

I 6

4 I

7 0.3 0.1 0.6 I

I 0

2 0

0.2 o.o 0.0 6

I 7

0. 1%

0,0"/o 0.1%

Shorthead reclmrse

  • I 6 7 0.6 II 8 5 24 2.0 31 0.4%

Channe I catfish 93 144 69 306 25.5 51 58 69 178 14.8 484 5.6%

Flathead catfish Banded killilish White perch 5

4 I

2 9

I 2

0.8

0. 1 0.2 4

I 3

.** 7 0

I 0.6 0.0 0.1 16 3

I 0.2%

+

+

Rock bass 16 58 51 125 10.4 3 14 5 22 1.8 147 1.7"/o Redbreast sunfish * *

  • 0 0.0 I
  • I 0.1 I +

Green sunfish P~ed Bluei:lll 64 60 I05 136 II 35 I

180 I

231 15.0 0.1 19.J 30 35 75 105 263 330 368 0

470 30.7 0.0 39.2 548 701 I

6.4%

+

8.1%

Smallmoulh bass Lar.:emoulh bass

\"11ile crappie 31 29 I

18 I

I 78 2

I 6.5 0.2 0.1 50 II 9

10 26 34 85 55 0

7.1 4.6 o.o 163 57 I

1.9"/o 0,7"/o

+

Black crappie Greensidc daner Tessellated daner I

8 5

I I

14 2

I 27 0.2 0.1 2.3 I

.* 0 0

I 0.0 0.0 0.1 2

28 I

+

+

0.3%

Banded daner Yellow perch Chesapeake logperrh 5 25 I

I 19 I

I 49

0. 1
0. 1 4.1 2

2 s 9 0

0 0.0 0.0 0.8 58 I

I

+

+

0.7%

Shield daner

  • 5 3 8 0.7 *
  • I I 0.1 9 0.1%

Walleye 21 II 15 47 3.9 17 10 2 29 2.4 76 0.9%

No. offish 1,130 653 451 2,234 186.2 2,576 2,469 1,330 6,375 531.3 8,609 99.9%

No. of Species 16 23 26 30 18 18 18 22 31 No. of Collections 4 4 4 12 4 4 4 12 24 No. offish/Collection 282.5 163.3 112.8 186.2 644.0 617.3 332.5 531.3 358.7 Diversily Index 1.47 2.30 2.63 0.52 0.69 1.71 Evenness Index 0.53 0.73 0.81 0.18 0.24 0.59 117

Final Report PBAPS Thermal Study Table 5-40. Summary of fisheries data collected by 1O' seine in Conowingo Pond, July through October 2010.

Non-thermaDv Affected Total Number/ Thennafto. Affected Total Number/

Tnxon 203 202 208 221 220 Nwnbcr Collection 214 21S Number CoDection Total  %

Gimmlshad 4 2 15 3 3 27 1.4 4 5 9 I.I 36 2.0%

Spotfin shiner 22 43 275 25 268 633 31.7 56 171 227 28.4 860 47.0%

Cornely shiner

  • 7
  • I 9 17 0.9 2S 7 32 4.0 49 2.7%

Spottail slmcr Swallowtail shiner 20 3

14 2 .* I 13 I

48 6

2.4 0.3 I

2 3

0 0.4 0.0 SI 6

2.8%

0.3%

Bluntnose minnow Creek chub Fallfish 8

I I

20 9

I 23 61 I

I

3. 1
0. 1 0.1 5

25 JO 0

0 3.8 0.0 0.0 91 I

I 5.0%

0.1%

0. 1%

QuilDJack White Sucker Northern hog sucker 2 3 5

2 4

2 7

5 6

0.4 O.J 0.3

  • 0 0

0 0.0 o.o 0.0 7

5 6

0.4%

0.3°/o 0.3%

Shorthead redhorse Channel catlsh Flathead catfish I

I I

I I

I

.*2 2

s I

0.3 0.1

0. 1

..* .** 0 0

0 0.0 0.0 0.0 s

2 I

0.3%

0.1%

0. 1%

Banded kiDifish 42 2S 9S 8 8 178 8~ 9 6

  • 6 0.8 184 10. 1%

Rock bass

  • 3
  • 2 I 6 0.3 *
  • 0 0.0 6 0.3%

Green sunfish 2 19 I

  • I 23 1.2 4 22 26 3.3 49 2.7%

Pwnpkinseed *

  • I *
  • I 0. 1 *
  • 0 0.0 I 0.1%

Bluegill 12 194 3

  • 74 283 14.2 10 48 58 7.3 341 18.7%

Smallmouth bass Largemouth bass Greenside daner I

I 5

2 I

4 2

s 7

2 12 0.4 0.1 0.6 I

0 I

0 o.o 0.1 0.0 7

3 12 0.4%

0.2%

0.7"/o Tessellated daner Bonded daner Chesaoeake loD~rch 9

34

.4 3

2 34 2

15 80 4

19 4.0 0.2 1.0

  • I 0

0 I 0. 1 0.0 0.0 81 4

19 4.4%

0.2%

l.O'Ye No. offish 127 378 410 93 427 l,43S 71.8 112 281 393 49.I 1,828 100.00/o No. of Species 14 19 12 14 IS 25 9 8 10 2S No. of CoDections 4 4 4 4 4 20 4 4 8 28 No. of Fish/Collection 31.8 94.S 102.S 23.3 106.8 71.8 28.0 70.3 49.I 6S.3 Diversity lnde>< 2.00 1.78 1.02 1.91 1.34 I.SI 1.24 Evenness lnde>< 0.76 0.6 0.41 0.72 0.49 0.69 0.6 118

Final Report PBAPS Thermal Study Table 5-41 . Summary by station of fisheries data collected by 16' Otter Trawl in Conowingo Pond July through October 2010.

McClellan's Rock Below Burkins Run BelowPBAPS Broad Creek PBAPS Intake Taxon 331* 332 333 381° 382° 383 384 371* 372 373 341 342 343 321 322 323 Total  %

Gizzanl shad l 7 4 *

  • 1 1 *
  • 2 12 20 6 8 *
  • 62 3.1%

Spotfin shiner

  • I * * * * * * * * * * * * *
  • l +

Common carp

  • 3 6
  • l
  • I
  • I
  • 4 3 7 3 *
  • 29 1.4%

Spottail shiner I 3 I * * * * * *

  • I * * * *
  • 6 0.3%

Quillback *

  • 2 * * * * * * *
  • I * * *
  • 3 0.1%

Northern hog sucker

  • I * * * * * * * * * * * * *
  • I +

Shorthead redhorse *

  • 3 * *
  • I * * * *
  • l * *
  • 5 0.2%

Channel catfish 255 473 173 21 41 205 43 3

  • 2 59 84 310 17
  • 45 1,731 85.8%

Flathead catfJSh

  • l I
  • I * * * * *
  • l * * *
  • 4 0.2%

White perch * * * * *

  • l * * *
  • I * * *
  • 2 0.1%

Rock bass *

  • l * * * * * * * * * * * *
  • l +

Bluegill Smallmoutb bass Largemouth bass 2

17 6

4 l l

2 2

I 3

6 1

16 4

6 4

s 78 2

l 3.9%

0.1°/a

+

White crappie * * * * * * * * * * *

  • l * *
  • I +

Tessellated darter l 25 8 3 6 *

  • 2
  • 2 19 I 4 15
  • 2 88 4.4%

Walleye

  • I I * * * * * * * *
  • I * *
  • 3 0.1%

No. of Fish 260 532 206 28 50 207 52 8 7 7 Ill 115 336 47 0 52 2,018 99.S°/o No. of Species 5 10 II 3 5 3 8 3 2 4 6 8 8 5 0 3 17 No. of Collections 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 4 64 No. ofFish/Collectior 65.0 133.0 51.5 7.0 12.5 51.8 13.0 2.0 1.8 1.8 27.8 28.8 84.0 11.8 00 13.0 31.5 Fish/10 minute haul 65.0 133.0 51.5 7.2 12.5 55.9 13.0 2.2 1.8 1.8 27.8 28.8 84 0 11.8 0.0 13.0 32.0 Diversity Index 0.12 0.52 0.77 0.73 0.65 0.06 0.79 1.08 0.41 1.35 1.32 0.91 0.40 1.42 0.00 0.48 0.66 Evemess looex O.D7 0.23 0.32 0.66 0.40 0.05 0.38 0.98 0.59 0.97 0.74 0.44 0. 19 091 000 0.49 0.23

  • Located within the i1fluence of PBAPS thennal effluent.

+Less than 0.05%.

119

Final Report PBAPS Thermal Study Table 5-42. Summary of fisheries data by station collected by boat electrofisher in February and April through October 2011.

Nor>-thennallv Affected Total Number/ Thermally Affected TOia! Number/

Taxon American shad Gizzard shad 164 2,136 16S 109 187 1,127 Number 0

3,372 Collection 0.0 140.5 161 1,697 189 821 190 217 1,089 3,118 I

Number I

6,725 Collection 0.0 231.9 Total I

10,097 55.7%

+

Spot&n shiner 193 20 588 801 33.4 75 120 67 55 317 10.9 1,118 6.20/o Corrnnon carp Conunon shiner .** 6 41 47 0

2.0 0.0 S9 20 22 2

II 112 2

3.9 0.1 IS9 2

0.9%

+

River chub Golden shiner Comely slmer 262 84 I

  • 2 l,22S I

2 l,S71 0.0 0.1 6S.S IS1 I

288 6

292 2

47 0

9 784 0.0 0.3 27.0 II I

2,3SS

+

0. 1%

13.0"lo Spottail shiner Swallowtail shiner Mimic shiner 29 8

34 2

I 40 6

103 I

16 4.3 0.0 0.7 38 I

IS 2

22 32 107 0

3 3.7 0.0 0.1 210 19 I

1.2%

0.1%

+

Bluntnose minnow Creek chub Fallfish 18 I

20 7

73 I

I Ill I

9 4.6 0.0 0.4

.* s

  • 20 100 I

29 I

9 I

158 2

6 5.4 0.1 0.2 269 3

IS I.SO/a

+

0. 1%

Qwllback White sucker Northern hog sucker I

  • 2 I

I s

3 7

4 2

0.3 0.2 0.1 10 2 2 I

I 14 I

I O.S o.o 0.0 21 5

3 0.1%

o.oo;.

+

Shorthead rcdhorse s 7 IS 27 I.I 14 s s 17 41 1.4 68 0.4%

Channel catfish Ill 125 ll3 371 15.S 176 109 101 94 480 16.6 851 4.7%

Flathead catfish Banded kiDifish 4

I s

I 2

I II 3

o.s 0.1 . .*

  • 10 8 3 I

2 23 I

0.8 0.0 34 4

0.2%

+

White pen:h Striped bass Hybrid Striped bass

.*I 19 4

20 0

4 0.8 0.0 0.2 2 3 I

I s

1 I

0.2 0.0 0.0 2S s

I O. J ~b

+

+

Rock bass 76 93 93 262 I0.9 6 20 19 37 82 2.8 344 1.9%

Redbreast sunfish * *

  • 0 0.0
  • I 3 3 7 0.2 7 +

Green slDlfish Pumpkinseed Bluegill 1S 65 42 86 13 86 130 0

237 S.4 0.0 9.9 129 77 I

SS 127 223 193 3S8 7

334 16S 8

731 26.4 0.3 25.2 89S 8

968 4 . ~~

5.3%

+

Smallmouth bass 115 56 42 213 8.9 44 25 40 23 132 4.6 345 1.9%

Largemouth bass While crappie Black crappie 4

I

.** 6 2

10 3

0 0.4 0.1 0.0 18 2

2 18 I

4 4

38 I

78 8

2 2.7 0.3 0.1 88 11 2

0.5%

0.1%

+

Greenside darter

  • 2
  • 2 0.1 I *
  • 2 3 0.1 5 +

Tessellated darter 2 2 2 6 0.3

  • 2 3 I 6 0.2 12 0. 1%

Yellow pen:h I 2 3 6 0.3 * *

  • 2 2 0.1 8 +

Chesapeake logpen:h Shield darter Walleye 11 1

20 10 9

14 20 I

35 II 40 1.5 0.5 1.7 18

.I 1 7

2 19 17 8

21 52 0

0.7 0.0 1.8 56 II 92 0.3%

0. 1'%

0.5%

No. ofFish 3,142 749 3,S48 7,439 310.0 2,S58 1.754 2,150 4,229 10,691 368.7 18,130 99.7%

No. of Species 22 28 28 36 23 24 23 30 29 38 No. of Collections 8 8 8 24 8 8 8 5 29 S3 No. of Fish/Collection 392.8 93.6 443.5 310.0 319.8 219.3 268.8 845.8 368.7 342.1 Diversity Index 1.31 2.52 1.76 1.43 1.85 1.73 I. II Evermess Index 042 0.76 0.53 046 0.58 0.55 0.33

+ Less than 0.05%.

120

Final Report PBAPS Thermal Study Table 5-43. Summary of fisheries data collected by 10' seine in Conowingo Pond, April through October 2011.

Non-thennallv Affected Toial Nwnbcr/ Thennallv Affected Total Nwnbcr/

Taxon 203 202 208 221 220 Nwnbcr Collection 214 215 Nwnbcr Collection Total  %

Gizzard shad 3

  • 12 13 3 31 0.9 7 4 II 0.8 42 2.6%

Spotfin shiner Common carp Common shiner 77 75 4

71 34 224 481 0

4 13.7 0.0 0.1 134 2

197 331 2

0 23.6 0.1 0.0 812 2

4 50.6%

0.1%

0.2%

Golden shiner *

  • 2 *
  • 2 0.1 I I 0. 1 3. 0.2%

Comely shiner Spottail shiner Mimic shiner II s

19 22 I

2 7

29 II 4

I 4

56 SS 5

1.6 1.6 0I 4

2 I

..2 6 2

I 0.4 0.1 0.1 62 57 6

3.9%

3.6%

0.4%

Bluntnose minnow IOS 28 23 22 IS 193 5.5 34 8 42 3.0 235 14.7%

Fallfish 5 2 *

  • 12 19 0.5 I I 0.1 20 1.2%

Quillbeck 2 51 I 7 I 62 1.8 0 0.0 62 3.9"/o Northern hog sucker Shorthead redhorse I

I 15 s

7 2

23 8

0.7 0.2 * .. 0 0

0.0 0.0 23 8

1.4%

0.5%

Channel <atfis h Eastern mosquilofish .* .

2

  • I I

I 4

I 0.1 0.0 . ..

6 6 0

0.4 0.0 IO 1

0.6%

0.1%

Banded killifish Hybrid Striped bass Rock bass I

I 8

24 I

.4 3

37 0

5 I.I 0.0 0.1 47 4

I I 47 2

4 3.4 0.1 0.3 84 2

9 5.2%

0.1%

0.6%

Green sunfish I

  • s
  • 4 10 0.3 4
  • 4 0.3 14 0.9"/o Bluegill 24 30 2 4 12 72 2.1 8 7 IS 1.1 87 S.4%

Smallmouth bass

  • 2 4 4 10 0.3
  • I I 0.1 11 0.7%

Large mouth bass Greensidc darter TesseDated darter 8

4 3

  • I 9 9 2 8

I 27 0.2 0.0 0.8 I

3 I

I 0

4 0.1 0.0 0.3 31 9

1 0.6%

0.1%

1.9"/o Yellow perch Chesapeake logpen:h Shield darter 4

I I

2 6 I

I 0.0 0.2 0.0 I

0 I

0 0.0 0.1 0.0 1

7 1

0.1%

0.4%

0.1%

No. offish 247 239 156 176 304 1.122 32. I 260 222 482 34.4 1.604 100.0%

No. of Species 12 13 19 14 17 24 16 8 18 26 No. of Collections 7 7 7 7 7 35 7 7 14 49 No. of Fish/Collection 35.3 34.I 22.3 25. I 43.4 32. I 37.1 31.7 34.4 32.7 Diversity Index 1.58 1.90 1.99 2.28 1.23 1.63 o.ss Evenness Index 0.64 0.74 0.67 0.86 0.43 0.59 0.26 121

Final Report PBAPS Thermal Study Table 5-44. Summary by station of fisheries data collected by 16' Otter Trawl in Conowingo Pond April through October 2011.

McClellan's Rock Below Burkins Run BelowPBAPS Broad Creek PBAPS Intake Taxon 331* 332 333 381* 382* 383 384 371* 372 373 341 342 343 321 322 323 Total  %

Alewife * * * * * * * * * * * *

  • I *
  • I +

Gizzanl shad Spot&n shiner 2

I I .

11

  • I I .

16 7 2

5 2

82 s . .

I *

  • I
  • .s
  • 126 12 2.1%

0.2%

Common carp Common shiner Golden shiler 4

4 3

I 9

I 6

1 1

2 4

I 22 3 4 I 2 78 I

I 1.3%

+

+

Comely shiner *

  • I
  • 3
  • 3
  • I 3 1 * *
  • 21
  • 39 0.7%

Spottail shiner 25 23 1 48 137 2 164 s 71 82 94 6 1 20 29 so 764 12.8%

Swallowtail shiner Bluntnose minnow .*

  • 1 37
  • 2 1

2 2

41

+

0.7°/o QuiDback White sucker Northern hog sucker I

1 1

2

.** I

  • 3 2

1 0.1%

+

+

Shorthead rcdhorse 2 *

  • 2 9 I 1 I I
  • s * * * *
  • 28 0.5%

Channel catfish 186 139 326 983 629 343 9 29 583 16 112 309 120 449 86 JS 4,354 73.1%

Flathead catfJSh I * * * * * * * *

  • 3
  • I * *
  • 5 0.1%

Rainbow smelt * * * * * * * *

  • I * * * * *
  • I +

White perch * * *

  • 1 1 *
  • 5 * * *
  • 2 I
  • to 0.2%

Hybrid Striped bass * * * * * * *

  • I
  • I * * * *
  • 2 +

Redbreast sunfJSh * * * * * * * * *

  • 1 * * * *
  • I +

Green sunf1Sh * * * * * * * * *

  • I * * * *
  • I +

Pumpkinseed

  • * * *
  • 2 * *
  • I * * *

. *

  • 3 0.1%

Bluegill 1 1 3 7 3 132 1 5 18 149 1 4 6 9 340 S.7%

Smallmouth bass Largemouth bass White crappie 1 4

  • 1 8

1 1 8 1

4 2

7 2 3 25 11 7

0.4%

0.2"/o 0.1%

Black crappie * * * * * * * *

  • I * * * *
  • 1 +

Tessellated darter I 3 I 13 8 I 14

  • 4 I 2 73 1.2%

Yellow perch * * * * *

  • 2 *
  • I
  • I *
  • 1
  • 5 0.1%

Chesapeake logperch * * * * * * * *

  • I * * *
  • 1
  • 2 +

Shield darter Walleve No. of Fish 223

  • I 173 I

351

.I 1,052 814 3

1 374 400 I

2 40 1 . .

689 3

146 I

1 509 322 131 485 143 104 11 5

5,956 0.2%

0.1%

99.7%

No. of Species 9 8 8 8 14 9 18 1 II 14 21 7 6 8 9 6 31 No. of Collections 1 1 7 1 7 1 1 1 7 1 1 1 1 1 1 1 112 No. of Fish/Collection 31.9 24.7 50.I 150.3 116.3 53.4 57.1 5.1 98.4 20.9 72.7 46.0 18.7 69.3 20.4 14.9 53.2 Fish/10 nmutc haul 31.9 24.7 50.1 150.3 116.3 55.0 57.1 6.1 98.4 21.5 76.0 46.0 18.7 71.3 20.4 14.9 53.8 Diversity Index 0.65 0.72 0.36 0.31 0.79 0.41 1.65 1.01 0.63 1.57 1.92 0.23 0.41 0.37 1.14 1.26 1.07 EveMess Index 0.30 0.35 0.18 0.15 0.30 0.19 0.51 0.52 0.26 0.59 0.63 0.12 0.23 0.18 0.52 0.70 0 31

  • Located within the influence of PBAPS thermal effluent.

+Less than 0.05%.

122

Final Report PBAPS Thermal Study Table 5-45. Summary of fisheries data by station collected by boat electrofisher in January, February, and April through October 2012.

Non-thennaOy Affected Total Number/ ThennaOy Affected Total Number/

Taxon Gizzard shad 164 1,160 165 326 187 875 Number 2,361 Collection 87.4 161 1,585 189 386 190 110 217 956 Number J,OJ7 Collection 84.4 Total 5,398 20.6%

Spottin shiner 70 12 JI 113 4.2 101 35 39 16 191 5.3 304 1.2%

Common carp Common shiner Golden shiner I

14 I

33 I

I 48 I

2 1.8 0.0 0.1 38 4

17 4

19 14 20 22 94 44 0

2.6 0.0 1.2 142 46 I

0.5%

+

O.?%

Comely shiner 3,486 762 214 4,462 165.3 58 2.215 2,338 211 4,822 133.9 9.284 3S.S%

Spot!Bil stmer IO 68 IOI 179 6.6 13 38 2S 8 84 2.3 263 1.0%

Rosyface shiner Minic shiner Bluntnose minnow 9

3 26 55 0

3 90 0.0 0.1 3.3

.8 I

  • 21 45 26 100 I

0 0.0 0.0 2.8 I

3 190 0.7%

+

+

Creek chub FaDfish 5

I I

3 I

9 2

0.3 0.1 .* 2 3

4 2

3 9

5 0.3

0. 1 18 7
0. 1%

+

QuiDback White sucker Nonhem hog sucker

.I I 2 I

2 8

5 3

9 8

0.1 O.J 0.3 .

5 I

I 4

I I

I 5

8 11 6

IO 0.2 0.3 0.3 20 9

18

+

O.l 'Yo 0.1%

Shorthead redhorse 2 II IOI 114 4.2 26 9

  • 79 114 3.2 228 0.9%

Channel catfish 88 140 132 360 13.3 199 118 165 173 655 18.2 1,015 3.9%

Flathead catf1Sh Tiger Muskellunge 5

3 8 16 0

0.6 0.0 4

I 5

7 3 19 I

0.5 0.0 35 I

0.1%

+

Atlanti: needlef1Sh White perch

  • .*
  • 4 0

4 0.0 0.1 19 s

  • I 20 5 0. 1 0.6 5

24

+

0.1%

Sttiped bass Hybrid Striped bass Rock bass 76 91 65 0

0 232 0.0 0.0 8.6 26 13 I

  • 3 26 2

24 29 65 I 0.0 0.8 1.8 I

29 297

+

0.1%

1.1%

Redbreast sunfish 5 I I 7 0.3 *

  • I 2 3 0. 1 10 +

Green s1mfish Pumpkmeed Blueglll 92 2

166 99 2

153 II I

110 202 429 5

7.5 0.2 15.9 90 282 48 I

157 275 1,467 I

650 2

4,443 1,063 4

6,349 29.5 0.1 176.4 1.265 9

6,778 4.8%

+

25.9%

Smallmouth ba.. 101 72 33 206 7.6 98 10 28 32 168 4.7 374 1.4%

Largemouth bau White crappie 10 I . .*

2 10 22 1

0.8 o.o 21 I

9 7

27 I

66 1

123 10 3.4 0.3 145 11 0.6%

+

Black crappie Greenside darter I

I I

I 0.0 0.0 .*2 I 3

I 6

I 0.2 0.0 7

2

+

+

Tessellated darter Yellow perch CheHpeake logperch I

  • I 6

5 12 15 6

13 21 0.2 0.5 0.8

. I 3

I 2

4 3

9 I

2 37 49 7

7 0.2 0.2 1.4 13 20 70 01%

0.3%

+

Walleve 13 23 17 SJ 2.0 37 17 4 4 62 1.7 115 0.4%

No. offish 5,306 1,821 1,856 8,983 332.7 2,640 3,145 4,592 6,798 17,175 477.1 26,158 99.7%

No. of Species 23 2S 29 30 2S 28 2S 27 32 35 No. of Collectims 9 9 9 27 9 9 9 9 36 63 No. offish/Collection 589.6 202.3 206.2 332.7 293.3 3494 510.2 755.3 477.l 415.2 Diversiy Index 1.63 2.80 2.91 2.32 1.75 1.97 1.83 Evenness Index 0.36 0.60 0.60 0.49 0.36 0.42 0.38

+Less than 0.05%.

123

Final Report PBAPS Thermal Study Table 5-46. Summary of fisheries data collected by 10' seine in Conowingo Pond, April through October 2012.

Non-thennallv Affected Total Nwnber/ Thennallv Affected Total Nwnber/

Taxon Giz:zanl shnd Rosyside dace 203 3

202 208 221 220 1

Nwnber 4

0 Collection 0.1 0.0 214 8

215 Nwnber 0

8 Collection o.o 0.6 Total 8

8 0.3%

0.3%

Spotfin shiner Cutlips minnow River chub 64 2

55 83 11 170 I

383 I

2 10.9 0.0 0.1 279 138 417 0

0 29.8 0.0 0.0 1,194 2

4 41.9"1.

0.1%

0. 1%

Comely shiner 6 10 3 15 23 57 1.6 15 II 26 1.9 142 5.0%

Spottail shiner 80 32 8 46 47 213 6.1 7 12 19 1.4 451 15.8%

Swallowtail shiner I * * *

  • I 0.0 *
  • 0 0.0 2 0.1%

Bluntnose minnow 15 26 6 69 77 193 5.5 19 25 44 3. 1 436 15.3%

Creek chub * * * *

  • 0 0.0 2
  • 2 0.1 2 0.1%

Fallfish Quillback White sucker 6

2 I

3 I

1 4 3

7 0.1 0.2 0.1 3

I 4 0

0 0.3 0.0 o.o 10 14 8

0.4%

0.5%

0.3%

Northern hog sucker 2 I 2 I 8 14 0.4 *

  • 0 0.0 28 1.0%

Shorthead redhorse I * *

  • I 2 0.1 *
  • 0 0.0 4 0.1%

Banded killif1Sh Hybrid striped bass Rock bass 22 I

41 2

5 65 0

6 1.9 0.0 0.2 I

0 I

0 0.0 0.1 0.0 132 I

12 4.6%

0.0%

0.4%

Redbreast swtfish Green sunf!Sh ..* *

  • 3 3

0 6

0.0 0.2 I

3 9

I 12 0.1 0.9 I

24 0.0%

0.8%

Bluegill Smallmouth bass Grecnside darter 1

9 1

11 I

2 27 2

49 4

I 1.4 0.1 0.0 8 51 1

59 1

0 4.2 0.1 0.0 158 9

2 5.6%

0.3%

0.1%

Tessellated darter Chesaoeakc loo"" rch No. ofFish 12 193 25 162 21 161 22 4

214 4

4 377 84 8

1,107 2.4 0.2 31.6 10 356 249 1

10 1

605 0.7 0.1 43.2 180 17 2,851 6.3%

0.6%

100.0%

No. of Species 12 10 II 10 17 20 II 9 13 24 No. of Collections 7 7 7 7 7 35 7 7 14 49 No. of Fish/Collection 27.6 23.1 23.0 30.6 53.9 31.6 50.9 35.6 43.2 58.2 Diversity Index 2.25 2.52 2.31 2.58 2.47 1.40 1.95 Evenness 0.63 0.76 0.67 0.78 0.60 0.39 0.62 124

Final Report PBAPS Thermal Study Table 5-47. Summary by station of fisheries data collected by 16' Otter Trawl in Conowingo Pond April through October 2012.

McClellan's Rock Below Burkins Run BelowPBAPS Broad Creek PBAPS Intake Taxon 331* 332 333 381* 382* 383 384 371* 372 373 341 342 343 321 322 323 Total  %

Gizzanl shad Spotfin shiner Conunon carp 3

I 1,088 9

84 17 8

I 8

5 170 274 12S I

  • 3 I
  • 93 9SO 5 6 29 3

IS I

102 3

28 4

6 12 4

II 7

2,986 16 75 46.0%

0.2%

1-2%

Comely shiner * * * * *

  • 3 *
  • I 2 * * * *
  • 6 0-1%

Spottail shiner

  • 4 *
  • 40 I 26 I 16 IO 95 I
  • 13 6 2 215 3.3%

Swallowtail shiner Bluntnose minnow 2

8 .*

s I

  • I I
  • .** .** 3 IS

+

0.2%

Quillback White sucker Shorthead redhorse

  • I I

3

  • 2
  • .I
  • 4 I 3 I

3 2

I

  • 3

. 2 7

17

+

0.1 %

0.3%

Channe I catfis b 4S 361 219 367 103 34 S2 90 S6 28 24 42 169 94 36 14 1,734 26.7%

Flathead catfish 2 I 2 * * * * *

  • I 2 I * * *
  • 9 0.1%

White perch

  • 3 I *
  • I *
  • 30 * *
  • 2 I *
  • 38 0.6%

Green swtf1Sh * * * * * * * * *

  • 3 * * * *
  • 3 +

Pwnpkinseed * * * * *

  • I * * * * * * * *
  • I +

Bluegill Smallmouth bass Largemouth bass S8 64 10 I

12 439 4

I .* .. .. . .** .**

s 4S 166 I

416 2

2 10 6 8 10 s

l,2S4 8

3 19.3%

0.1%

+

White crappie *

  • I * * * *
  • I +

Tessellated darter 3 8 I 2 9 6 4 3 19 I 8 9

  • 2
  • 8 83 1.3%

Yellow perch * * * * *

  • 2 * *
  • I * * * *
  • 3 +

Chesapeake logpen:h Woline No. offish 54 1,475 385 I . .

450 343 I

330 667 104 275 1,169 594 I

80 282 I

154 75 I

2 49 I

6 6,486

+

0.1%

99.7%

No. of Species 5 8 IO 6 9 8 12 7 II 12 16 8 5 9 7 7 23 No. of Collectims 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 7 112 No. of Fish/Collection 7_7 2I0.7 55.0 64.3 49.0 47.l 95.3 14.9 39.3 167.0 84.9 11.4 40.3 22.0 I0.7 7.0 57.9 Fish/IO minute haul 7.7 216.9 55.0 64.3 49.0 47.1 95.3 17.0 39.3 167.0 84.9 11.4 40.3 23.3 11.0 7.0 58.8 Diversity Index 0.97 0.96 1.70 0.90 2.14 0.94 1.60 0.88 2.64 0.94 1.57 1.99 1.21 1.83 2.21 2.54 1.99 Evenness Index 0.42 0.32 0.51 0.35 0.67 0.31 0.45 0.31 0.76 0.26 0.39 0.66 0.52 0.58 0.79 0.91 0.44

  • Located within the influence of PBAPS thermal effluent Less than 0.05%.

125

Final Report PBAPS Thermal Study Table 5-48. Summary of fisheries data by station collected by boat electrofisher in January, March, and April through October 2013 Non-thermaDv Affected Total Nwnbcrl ThennaDv A!Tected Total Nwnbcrl Taxm 164 165 187 Number Collection 161 189 190 217 Number Collection Total  %

Girzanl shad 8S SS 116 2S6 9.S 1,988 92 16S S39 2,784 77.J 3,040 19.6%

Spot&n shiner 121 16 IS8 29S 10.9 2S3 119 110 17 499 13.9 794 S.1%

Grass carp * *

  • 0 0.0 1 * *
  • 1 0.0 1 +

COllUllOll carp 2 6 13 21 0.8 67 6 9 4 86 2.4 J07 0.7%

Golden shiner

  • 1
  • I 0.0 2 2 3 12 19 0.5 20 0.1%

Comely shiner 362 212 286 860 31.9 325 114 318 199 956 26.6 1,816 11.7%

Spottail shiner 26 37 173 236 8.7 12 70 14 36 132 3.7 368 2.4%

Swallowtail shiner Mimic shiner Bluntnose minnow 67 198 2

I 182 1

2 447 0.0 0.1 16.6 SI 100 279 1

112 I

0 S42 0.0 0.0 IS.I 2

2 989

+

+

6.4%

Creek chub 1

  • 1 2 0.1
  • 5 4
  • 9 0.3 11 0. 1%

Fallf1Sh Quillback White sucker

  • 3 I

0 3

I 0.0 0.1 o.o 1

1 2

1 2

4 1

2 0.1 0.0 0.1 4

4 3

+

+

+

Northern hogsucker 3 3 0.1 * *

  • I 1 0.0 4 +

Shorthead redhorse 4 12 178 194 7.2 32 14 1 52 99 2.8 293 1.9%

Channel catfish 110 129 146 38S 14.J 94 149 177 122 S42 IS.I 986 6.4%

Flathead catfish 8 5 3 16 0.6 13 9 I I 24 0.7 40 0.3%

Muskellunge Brown trout Bandcdkillilish 4 4

1 6

0 1

14 0.0 0.0 0.5 I

I I

I I

I I

I 4

0.0 0.0 0.1 I

2 18

+

0.0%

0.1%

White perch Striped bass x white bass Rock bass 95 1

121 19 111 20 0

327 0.7 0.0 12.1 26 5

13 2

36 3

32 28 5

84 0.8 0.1 2.3 48 5

411 0.3%

+

2.6%

Redbreast sunfish 7 I I 9 0.3 4 * *

  • 4 0.1 13 0. 1%

Green sunfish 174 172 34 380 14.1 279 186 593 221 1,279 35.5 1,659 J0.7%

PumpkBtseed 5 3 2 JO 0.4 4

  • 1 4 9 0.3 19 0. 1%

Bluegill 226 294 2S3 773 28.6 474 369 492 899 2,234 62.1 3,007 19.4%

Smallmouth bass 273 141 142 SS6 20.6 186 67 130 128 Sil 14.2 1,067 6.9%

Largemouth bass 12 2 13 27 1.0 37 23 2S 34 119 3.3 146 0.9°/o White crappie

  • 3 s 8 0.3 s 6 I 2 14 0.4 22 0.1%

Black crappie * *

  • 0 0.0 7 2 *
  • 9 0.3 9 0.1%

Greensidc darter I 5

  • 6 0.2 3 1 4 II 19 0.5 25 0.2%

Tessellated darter 5 9 20 34 1.3 I JO 15 33 59 1.6 93 0.6%

Yellow perch 6 11 60 77 2.9

  • 9 3 9 21 0.6 98 0.6%

Chesapeake logperch 8 70 70 148 s.s 16 6 42 9S IS9 4.4 369 2.4%

Shield darter

  • 17 2 19 0.7
  • 2 1 11 14 0.4 33 0.2%

Walleve IS 12 40 67 2.S 14 7 14 7 42 1.2 109 0.7%

No. ofFish 1,617 1,541 2,041 5,199 192.6 3,915 1,411 2,406 2,586 10,318 286.6 15,517 100.6%

No. of Species 23 28 29 38 29 29 25 28 38 38 No. of collections 9 9 9 27 9 9 9 9 36 63 No. off15h/Collection 179.7 171.2 226.8 192.6 435.0 156.8 267.3 287.3 286.6 246.3 Diversity Index 3.33 3.53 3.85 2.61 3.48 3.11 3.09 Evencss 0.74 0.73 0.79 0.54 0.72 0.67 0.64

+ Less than 0.05%.

126

Final Report PBAPS Thermal Study Table 5-49. Summary of fisheries data collected by 1O' seine in Conowingo Pond, April through October 2013.

Non-thennallv Affected Total Nwnber/ Thennallv Affected Total Nwnber/

Station No. 202 203 208 220 221 Nwnber Collection 214 215 Nwnber Collection Total  %

Gizzard shad

  • 4 4 0.1 *
  • 0 0.0 4 0.1%

Spotfin shiner 67 50 45 120 12 294 8.4 135 151 286 20.4 580 20.9%

Central stoneroller * * *

  • I I 0.0 2
  • 2 0.1 3 0.1%

Comely shiter Common shiner 38 27 4

10 26 I

105 I

3.0 0.0 13 22 . 5 18 22 1.3 1.6 123 23 4.4%

0.8"/o Spottail shiner Swallowtail shiner 114 2 . . .

82 6 63 92 357 2

10.2 0.1 5

15 20 0

1.4 0.0 377 2

13.6%

0.1%

Bluntnose minnow 66 64 68 79 156 433 12.4 42 22 64 4.6 497 17.9%

Blacknose dace Creek chub I .* 0 I

0.0 0.0 I

I 0

0.1 0.0 I

I

+

+

Quillback White sucker Northern hogsucker 4

I II 2

I 2

2 2

4 94 3

I 22 99 6

0.6 2.8 0.2

  • 0 0

0 0.0 o.o 0.0 22 99 6

0.8"/o 3.6%

0.2%

Shorthead redhorse Channel catfish 3

I

  • 3 4

3 0.1 0.1 I

I I

I 0.1 0.1 4 5 0.2%

0.1%

Banded killifish White perch . .* . .

9 18 51 3 314 395 0

11.3 0.0 218 I

218 I

15.6 0.1 613 I

22.1%

+

Rock bass Green sunfish Bluegill 117 I

I I

14 29 4

4 69 I

6 18 217 0.2 0.5 6.2 I

19 3 22 0

I 0.0 0.1 1.6 6

19 239 0.2%

0.7%

8.6%

Smallmouth bass Large mouth bass Greenside darter 10 6 9 2

2 11 I

3 39 3

2 I.I 0.1 0.1 4

14 18 0

0 1.3 0.0 0.0 57 3

2 2.1%

0.1%

0.1%

Tessellated darter Yellow perch 6

3 5

I 14 6

I .

10 41 5

1.2 0.1 3

3 6

0 0.4 0.0 47 5

1.7%

0.2%

Chesapeake logpen:h Shield darter No. offish 442 I

269 8

5 262 19 401 I

I 719 29 6

2,093 0.8 0.2 I

467 215 I

0 682 0.1 0.0 30 6

2,775 1.1%

0.2%

100 No. of species 15 13 16 17 16 27 14 9 27 27 No. of Collections 7 7 7 7 7 35 7 7 14 49 No. of fish/Collection 63.1 38.4 37.4 57.3 102.7 59.8 66.7 30.7 48.7 56.6 Diversity Index 2.71 2.82 3.04 2.79 2.30 1.99 1.62 Eveness 0.69 0.81 0.78 0,71 0 57 0-54 0.54

+ Less than 0. 05%.

127

Final Report PBAPS Thermal Study Fish Metrics and CPUE Comparison of CPUE and community based metrics among collection locations is useful in describing differences in the fish community among stations. Gear specific CPUE normalizes the catch based on level of effort and, therefore, allows standardized comparisons of relative abundance. Several metrics that describe the fish community at individual stations were calculated for the seine and electrofishing collections. No analysis is provided for the trawl collections; the rationale for this decision was discussed previously.

For this analysis stations are discussed as either non-thermal or thermal based on their location in relation to the PBAPS thermal plume. Stations downstream of the discharge canal that experience elevated water temperatures above ambient water temperature for the entire collection period are considered to be thermally influenced. Stations that are upstream of the PBAPS thermal discharge that experience natural water temperature conditions are considered non-thermal (Figure 5-22 to Figure 5-24; Table 5-12 to Table 5-14). Electrofishing Stations 161, 189, 190, and 217 are considered thermally influenced and Stations 187, 164, and 165 are considered non-thermal. Seine Stations 214 and 215 are considered thermally influenced and Stations 203, 202, 220, 221, and 208 are considered non-thermal. As previously discussed in Section 5.2, Station 208 does experience elevated water temperatures during a portion of the year resulting from thermal plume movement upstream during low flow conditions. However, this station is considered non-thermal because it does not experience a prolonged thermal influence.

Monthly metric values were compared among locations to determine if statistical differences existed between individuals stations. A total of five metrics were calculated including overall CPUE, species richness, RIS richness, Shannon diversity, and evenness. Differences in metrics values among stations were assessed using the nonparametric Kruskal-Wallis test. This nonparametric test was selected for these analyses rather than the analogous parametric ANOVA test because not all test groups met the assumptions of equal variances, normal distribution, and equal sample size among the stations. The nonparametric test was used for all analyses to streamline statistical analysis among the test metrics.

Mean CPUE by month is provided for several RIS collected using both seine and electrofishing.

Species that were collected in low numbers for a specific gear type were excluded from analysis because insufficient numbers of individuals were collected to make meaningful comparisons among stations or months. Catch results for White Sucker and White Crappie were not included for either gear type because insufficient numbers of individuals were collected to make meaningful comparisons among stations or months for either gear type.

A two-way analysis of variance (ANOVA) was performed on electrofishing data collected from July through October 2010-2013 to detect differences in the CPUE between stations and years.

The analysis was conducted on several of the RIS: Gizzard Shad, Spotfin Shiner, Smallmouth Bass, Channel Catfish, and Bluegill. Other designated RIS were collected sporadically throughout the period and, because of sporadic collection, it was judged that statistical analysis 128

Final Report PBAPS Thermal Study would not provide useful information for them . Data from the seine sampling was similarly treated due to low numbers collected and/or collections where no fish were taken.

Indices of diversity and evenness were calculated to describe fish community structure. Species diversity (D) was calculated by the Shannon-Weaver (1948) method using the formula:

s D= -L P;Log 2 P; i= I Where:

D is the species diversity index, S is the total number of species collected, and P; is the proportion of a species in the sample.

Since the number of species varies between stations and months, an index of evenness was also calculated using the formula (Pielou 1966):

E = H'/H'max Where:

H' is the diversity and H'max is the log of the number of taxa.

Evenness values have a range from 0 to 1.0, with 1.0 being the maximum equality for a community.

E/ectrofishinq Results Five metrics were calculated to provide a description of the fish community among stations and across monthly collections in Conowingo Pond from April to October 2010-2013. Figure 5-42 through Figure 5-46 provide box plots which illustrate the spread of metric values among stations. Table 5-50 through Table 5-54 provide mean and median values for each metric among the stations. Square root transformed mean CPUE was similar among stations with highest CPUE observed at Station 217 {Table 5-50). Station 217 median CPUE was significantly higher (p<0.05) than Station 165 (non-thermal) and Station 189 (thermal).

Otherwise, CPUE was similar among stations. Species richness was similar among stations with mean values <!!12 for all stations. Generally the highest richness values were observed at Station 187 (non-thermal) and Station 217 (thermal) with median richness values for several stations significantly different (p<0.05) from these two stations (Table 5-51). Similar to species richness, RIS richness was highest at Stations 187 and 217. RIS richness for Stations 187 and 217 was significantly different (p<0.05) from several stations (Table 5-52). Shannon diversity values were highest at Station 187 with this station scores being significantly different (p<0.05) than Stations 164, 161, 190, and 217. The lowest Shannon diversity mean and median values 129

Final Report PBAPS Thermal Study were observed at Station 161. Similar to Shannon diversity, evenness values were highest for Station 187 with this station being significantly different (p<0.05) than Stations 217 and 161 (Table 5-54). Other significant differences in median evenness values were observed between other non-thermal and thermal stations.

Seasonal Patterns Figure 5-47 through Figure 5-51 provide box plots which graphically illustrate the spread, central tendency, and distribution of the five metrics by station for each monthly collection. Square root transformed CPUE was variable among stations and months with most catches between 100-900 fish/0.5hr. No obvious patterns were related to location, within or outside of the thermal plume during the course of the field season. Species richness was quite variable depending on month of collection (Figure 5-48). For most stations species richness increased over the course of the season with highest richness observed during September and October. Station 161 richness was lower in July; roughly 5-10 fewer species were observed during this month compared to other months. RIS richness ranged generally from 5 to 9 species per month for all stations. No well-defined seasonal patterns were evident (Figure 5-49). Similar to species richness, RIS richness at Station 161 was lowest in July. Shannon diversity values were quite variable among stations and months (Figure 5-50). Shannon diversity was generally highest from August through October for most stations. Similar to Shannon diversity, evenness was variable among stations and months and generally ranged between 0.5 and 0.9 (Figure 5-51).

Station 161 exhibited variable evenness among months with the highest values in June and October, and much lower values in April. During other months evenness was variable at this station.

RIS CPUE Mean electrofishing CPUE by station and month for the RIS is provided in Table 5-55 through Table 5-63. Mean CPUE for most RIS varied widely between stations and collection month including Gizzard Shad, Spotfin Shiner, Channel Catfish, Bluntnose Minnow, Bluegill, and Smallmouth Bass. CPUE was generally low for Largemouth Bass, Chesapeake Logperch, and Walleye. Gizzard Shad mean CPUE was highest in July and August for most stations. This is likely due to large numbers of YOY growing to sufficient size to be collected with electrofishing gear (recruited to the gear). Gizzard Shad mean CPUE was low for all months at Station 165 (non-thermal) and highest at Station 161 (thermal). Spotfin Shiner catch was lowest for Stations 165 and 217. No seasonal patterns were observed among the stations for this species. Higher catch rates were observed at Station 161 and Station 189 during May and June and Stations 164 and 187 in June and July. CPUE for Bluntnose Minnow showed no distinct patterns among - -- - -

stations or collection months. The highest mean CPUE for this species was observed at Station 190 in May. Channel Catfish CPUE was similar among stations and collection month. No specific patterns were observed for this species. Bluegill CPUE generally was highest during August through October. The highest overall CPUE was observed at Stations 217 and 190, both thermally influenced. Smallmouth Bass CPUE was variable among stations and collection month. CPUE was highest in September and October for Stations 164, 165, and 161 and highest in July for Stations 190 and 217. Largemouth Bass CPUE was generally low for all 130

Final Report PBAPS Thermal Study stations, and in particular, for the non-thermal stations during April through August. Seasonal patterns in Largemouth Bass distribution were clearly evident with high CPUE observed in September and October for Stations 189, 190, and 217. Chesapeake Logperch CPUE was low for all stations and most months. The highest catch rates occurred at Station 217 in August and September and at Station 187 during August through October. Walleye CPUE was fairly low for most stations from April to August. Seasonal patterns of higher Walleye catch rates were observed during October for all stations except Station 190 which had highest CPUE during April.

The results of the ANOVA performed on the electrofishing CPUE for select RIS showed significant differences (p <0.1) for several species between years, stations, and for station and year interaction. Gizzard Shad CPUE was significantly different across years with low CPUE in 2013 compared to the other years. No significant differences were observed for Gizzard Shad catch among stations or when accounting for station and year interaction. Smallmouth Bass CPUE was significantly different among years with higher catch in 2013 compared to previous years and with significantly different catches observed for several stations. CPUE tended to be higher for Stations 161, 164, 165, and 217. Bluegill CPUE was significantly different among years, stations, and for station and year interaction. Higher Bluegill CPUE was observed during 2012 and 2013 at Stations 190 and 217. Spotfin Shiner and Channel Catfish CPUE were not significantly different among years or stations. Although statistically significant differences were observed, the variation observed between years and stations was likely due to the natural variation inherent in the species' populations and variation in environmental conditions within Conowingo Pond.

Winter Metrics Winter electrofishing was completed during 2011 through 2013 to document seasonal differences in fish community composition. A total of five collections were completed at each station in January 2011 and 2013, February 2011 and 2012, and March 2013. Five metrics were calculated to characterize fish community during this season. CPUE was variable among months with highest catch observed at non-thermal Station 164 (Table 5-64). Species richness was highest each month for thermally influenced Station 161, where typically five or more additional species were collected as compared to the non-thermal stations (Table 5-65). In addition, for each station more species were collected during March than in the other months.

Similar to species richness, RIS richness was high at Station 161 for each month of winter collections (Table 5-66). RIS richness was also high at thermally influenced Station 189 during January and March. Shannon diversity values were highest at Station 161 for each month and also high at Station 189 for January and March (Table 5-67). Low Shannon diversity values were observed at Station 164. Similar to Shannon diversity, evenness was high at Station 161 during each month and low at Station 164 for each month (Table 5-68). Table 5-69 provides winter CPUE of Gizzard Shad. Gizzard Shad catch was low for most stations and months with the highest catch observed at thermal Station 161 in February and March and Station 189 in January.

131

Final Report PBAPS Thermal Study Seine Results Five metrics were calculated to provide a description of the fish community among stations and across monthly collections in Conowingo Pond from April to October 2010-2013. Figure 5-52 through Figure 5-56 provide box plots which illustrate the spread of metric values among stations. Table 5-70 through Table 5-74 provide mean and median values for each metric among the stations. Square root transformed mean CPUE was similar among stations with highest CPUE observed at Station 220 (Table 5-70). Station 220 median CPUE was significantly higher (p=0.1) than CPUE at Station 221 (non-thermal). Otherwise, CPUE was similar among stations. Species richness was similar among stations with mean values greater than five species for all stations except Station 215 (thermal). Generally the highest richness values were observed at Station 220 (non-thermal) with only thermally affected Station 215 significantly different (p=0.05) from Station 220 (Table 5-71). Similar to species richness, mean RIS richness was highest at Station 220. No significant differences in RIS richness were observed among the stations (Table 5-72). Shannon diversity values were similar for most stations with median values at Station 221 (non-thermal) being significantly different (p = 0.09) than Station 215 (thermal) (Table 5-73). Evenness values were comparable among stations with no significant differences observed (Table 5-74).

Seasonal Patterns Figure 5-57 through Figure 5-61 provide box plots which graphically illustrate the spread, central tendency, and distribution of the five metrics by station for each monthly collection. Square root transformed CPUE was variable among stations and months with most catches between 16-64 fish/collection. No obvious patterns were observed related to location within or outside of the thermal plume during the course of the field season. Species richness was quite variable depending on month of collection. For most stations species richness showed no distinct pattern over the course of the field season; however, species richness tended to be higher for several stations in August. At thermally influenced Stations 214 and 215 richness was lower in July and/or August when roughly one to three fewer species were observed as compared to other months. RIS richness usually ranged from one to four species per month for all stations with RIS richness typically lowest in April. Shannon diversity values were quite variable among stations and months with widely varied interquartile ranges. Shannon diversity was generally lower at Stations 214 and 215 during June and July compared to other months at these locations. Similar to Shannon diversity, evenness was variable among stations and months and generally ranged between 0.5 and 0.8. The interquartile range varied widely among months and stations.

RIS CPUE Mean seine CPUE by station and month for select RIS is provided in Table 5-75 through Table 5-79. Many of the RIS are usually not collected using a seine and were not included in this analysis. Spotfin Shiner and Bluntnose Minnow were the most common and consistently collected species among stations and months. Spotfin Shiner mean CPUE was generally the highest for most stations from July through October. Mean CPUE for this species was similar at the thermal stations (Stations 214 and 215) and at the non-thermal stations. No reduction in 132

Final Report PBAPS Thermal Study Spotfin Shiner CPUE was observed during July or August. Bluntnose Minnow mean CPUE was variable among stations and months. CPUE for Bluntnose Minnow showed no distinct patterns among stations. Additionally, no reduction in CPUE was observed during July or August at the two thermal stations. Bluegill mean CPUE varied widely among stations and months with the highest catches observed during August and September. Smallmouth Bass CPUE was generally low for all stations and months with no discernable pattern related to location or month of collection. Similar to Smallmouth Bass, Chesapeake Logperch CPUE was low for all stations and most months. The highest catch rates occurred at Station 220 in July and August.

Discussion The community metrics and CPUE provide a description of the fish community both spatially (station) and temporally (month) within Conowingo Pond. The electrofishing results illustrate variation in the data across stations and months. The metrics indicate that fewer fish species were present at Station 161 during July and in some years during August. Fishes likely avoided this area because of the elevated water temperatures resulting from the PBAPS thermal discharge. Station 161 is the station closest to PBAPS and experienced the highest water temperatures observed at the electrofishing stations. This avoidance was of short duration given that community metrics improved at this station during the subsequent months (August through October). Patterns of avoidance were not readily apparent from the monthly metric values for the other thermally affected electrofishing stations. However, Shannon diversity and evenness values tended to vary more widely at the thermal stations as compared to the non-thermal stations.

On the whole (across all months) the fish community diversity and relative abundance was similar regardless of collection location. Specific locations (i.e. Stations 187 and 217) tended to have greater diversity, likely related to greater habitat diversity or habitat preference. However, the avoidance observed at the near-field station was of short duration followed by greater numbers of species being collected in subsequent months. Community heterogeneity and relative abundance of the RIS was comparable during all months but July and August at Station 161. In fact, community heterogeneity was higher at Station 161 during January through March compared to all other stations. A cyclical pattern was observed, but not a substantial reduction in community heterogeneity at Station 161 as compared to the other stations.

Fewer species were collected by seine than were taken by electrofishing. The RIS CPUE for seine collections did not reveal any apparent patterns among the stations or related to month of collection with the exception of Stations 214 and 215. Several metric values indicated a pattern of lower values during June and July at thermally influenced seine Stations 214 and 215, which experienced elevated water temperatures that are typically highest in July. Species richness, Shannon diversity, and evenness values were lower at these stations during June and/or July indicating potential avoidance of these areas during at least one year of the study.

For both electrofishing and seining collections, metric values and RIS CPUE were useful in evaluating differences in the fish community and relative abundance of RIS across locations and months of collection. Fish tended to avoid stations that experienced the highest water temperatures during the summer months. This was most clearly evident at electrofishing 133

Final Report PBAPS Thermal Study Station 161 in July where for each year of the study five to ten fewer species were collected as compared to other months. Avoidance was also observed at seine Stations 214 and 215 during June and/or July for in at least one year of the study. RIS CPUE for both electrofishing and seining varied widely across stations and months and did not reveal any discernable patterns of lower catches during the summer months at Stations 161, 214, or 215. Although avoidance occurred at these locations, community composition quickly rebounded in subsequent months when water temperatures decreased and fish repopulated these areas. No long-term avoidance or loss of community structure was observed at the electrofishing or seine stations.

In contrast to summer avoidance, winter electrofishing indicated that fish appeared to be attracted to the warmer temperatures at Station 161. High species richness was observed at this station compared to the other thermal and non-thermally influenced locations.

Gizzard Shad Potential as Nuisance Species Gizzard Shad is native to the Atlantic and Gulf slopes and to interior drainages of eastern and central North America (Jenkins and Burkhead 1994). The lower Susquehanna River likely represented the historic northern-most range of this species. In 1972 Gizzard Shad was introduced into Conowingo Pond via the Conowingo Dam Fish Lift. Since 1972 over 30 million individuals have been lifted into the Pond. Gizzard Shad abundance has been increasing in the Chesapeake Bay region since the late 1980's and may be indicative of reduced habitat quality in the Bay (MDDNR 2013). Over the current 4-year study period approximately 3.2 million Gizzard Shad were passed into the Pond via the Conowingo Dam East Fish Lift. These pre-spawn adult fish produced large numbers of young that were observed in the catch data during the summer for this study.

A general concern with Gizzard Shad is the potential for this species to increase to such high numbers that it becomes a nuisance species within Conowingo Pond. The Gizzard Shad is a cold-intolerant species that can experience overwinter mortality at water temperatures less than approximately 4°C (Fetzer et al. 2011). The implication is that the PBAPS thermal plume may provide a winter refuge for this species, which leads to a larger population size than would exist without PBAPS. Young Gizzard Shad compete with young of many Centrarchids for zooplankton and may depress their numbers and growth rates in the Pond. Thus a larger population of this species may have an effect on relative abundance of other important recreational fish species. For example, the introduction of Gizzard Shad into the Pond has previously been linked to decline in the White Crappie population (RMC 1994). However, Gizzard Shad at present is common in areas upstream of PBAPS without the influence of thermal discharges (Figure 5-62).

The winter electrofishing catch is provided in Table 5-69 for Gizzard Shad. Gizzard Shad mean CPUE was much lower in the winter for all stations compared to collections from April through October (Table 5-55). The highest catch rates occurred during July and August with generally much lower CPUE in June and during the winter months. One might expect a cold intolerant species to benefit from warm water during winter months particularly when ambient water temperatures decrease below 4°C. The CPUE data at the thermally influenced Stations 161, 189, and 190 did not indicate the presence of large numbers of Gizzard Shad during the winter 134

Final Report PBAPS Thermal Study months. The winter CPUE results do not support a conclusion that the PBAPS thermal plume is interfering with the fall outmigration of Gizzard Shad or attracting excessively large numbers of this species during the winter months and, thus, providing a thermal refuge. In addition, during the fall large numbers of Gizzard Shad have been observed emigrating from Conowingo Pond downstream past Conowingo Dam. However, the higher winter time water temperature created by PBAPS would likely provide for conditions that are more suitable to this species, particularly during extremely cold winter periods, for those individuals that remain in the Pond. The annual migration (fish lift introductions) of Gizzard Shad from the lower Susquehanna River likely contributes substantially to the total population of this species in the Pond, and these fish did not benefit from overwintering in the Pond within the extent of the PBAPS thermal plume.

A parallel to the increase of the Gizzard Shad population in Conowingo Pond has been observed in many northeastern rivers within the United States. Similar to the Conowingo Pond, Gizzard Shad was first collected in the 1970's from the Hudson River (1974) (Daniels et al.

2005). The tidal Hudson River Gizzard Shad numbers have been documented to be increasing in abundance (Daniels et al. 2005). Gizzard Shad have been reported in other northern rivers including the Connecticut, Merrimack, and Kennebec rivers, suggesting that this species is expanding its range northward. Gizzard Shad have been present in the Delaware River Estuary since the 1960's and anecdotal evidence indicates the population has been expanding since that time into the Delaware and Schuylkill River drainages in Pennsylvania. The region-wide range expansion in the northeast and range expansion in other northern areas of the United States has been linked to increased water temperature potentially resulting from climate change (VanDeHey et al. 2011, Gephard 2005).

Chesapeake Loqperch Chesapeake Logperch (Percina bimaculata) was recently listed as threatened in Pennsylvania.

Its current range includes the Chesapeake Bay watershed in Maryland and Pennsylvania, limited to lower sections of the Susquehanna River and tributaries in Maryland and Pennsylvania, and a few direct tributaries to the Chesapeake Bay (Jenkins and Burkhead 1994).

In Pennsylvania, it is restricted to the Susquehanna River above and below Conowingo Dam and the lowermost sections of four tributaries to Conowingo Pond including Fishing Creek, Muddy Creek, Peters Creek and Michaels Run located in Lancaster and York Counties. It is also found in the Octoraro Creek in Chester and Lancaster Counties below Conowingo Dam. In Maryland, this species is known to inhabit the lower reaches of Broad, Conowingo, Deer, and Octoraro creeks.

--- - - Although relatively little is known about the Chesapeake Log perch, its habits and biology are - - --

likely to be similar to those of other logperches, in particular, the Logperch Percina caprodes.

Log perch spawning occurs from mid-March to mid-July (initiated at water temperature of 10-150C) over clean gravel or sand in swift currents of streams and near shores of lakes (Jenkins and Burkhead 1994). It is unclear whether Chesapeake Logperch spawn along the shores of the Conowingo Pond or if spawning is restricted to the lower sections of the six tributary streams of the Pond with documented occurrence of the species (Fishing Creek, Muddy Creek, Michaels Run, Peters Creek in Pennsylvania; Broad and Conowingo Creek in Maryland). Logperch have 135

Final Report PBAPS Thermal Study been observed to move from shallow areas into deeper water during the winter and migrate back into shallow areas prior to spawning (Winn 1958).

Seasonal and Spatial Distribution In this study, electrofishing proved more effective in collecting Chesapeake Logperch than seining. Very few Chesapeake Logperch were taken by trawling. Electrofishing catch data indicate that Chesapeake Logperch occurrence in the Pond varies through the year (Table 5-62). Only two Chesapeake Logperch were collected during the winter (January-March 2011-2013) from the Pond. A single individual was collected from both Stations 190 and 217 during 2013. Electrofishing CPUE was low from April to June and increased during the summer months with highest CPUE occurring from August through October. Chesapeake Logperch electrofishing CPUE was variable among collection locations (Table 5-62). The highest CPUE was observed at two non-thermal Stations, 165 (upstream from Peters Creek) and 187 (downstream from Muddy Creek), and one thermally influenced Station, 217 (upstream of Conowingo Creek). Otherwise, catch was lower for most months at the other four electrofishing locations including Station 161 (upstream from Michaels Run) which is the thermally influenced station closest to PBAPS. Few Chesapeake Logperch were collected while seining in Conowingo Pond and overall catch rates were low (Table 5-79). Similar to electrofishing results, the highest CPUE was observed during August. Seine catches were highest at Station 220, which is downstream of Muddy Creek, and Station 208, which is downstream of Peters Creek. Few Chesapeake Logperch were collected at the two thermally influenced seine locations (Stations 214 and 215) or the two most upstream non-thermal locations (Stations 202 and 203).

Discussion The life cycle of the Chesapeake Logperch in the Pond and its tributaries is not well known.

The distribution of this species within the Pond did not seem random, with higher catch rates at several stations and lower catch at most of the other stations. Distribution seems to be, in part, related to proximity to tributary streams and shallow shoreline habitat. CPUE was highest at electrofishing Station 187 and seine Station 220 (both downstream from Muddy Creek),

electrofishing Station 164 and seine Station 208 (both near Peters Creek), and electrofishing Station 217 (upstream from Conowingo Creek). Within these shallow shoreline areas, Chesapeake Logperch are likely selecting for a specific habitat composition (e.g., presence of sand, clean gravel, SAV, complex structure, woody debris) for both protective cover and feeding opportunity.

CPUE of Chesapeake Logperch was low at the sampling stations closest to the PBAPS that experience the highest water temperatures, i.e., Stations 161, 214, and 215. Catch at these locations was low throughout most of the sampling season with higher CPUE during September and October. However, the closest tributary to these stations with known Chesapeake Logperch occurrence is Michaels Run which is approximately 1.2 miles downstream from Stations 161 and 215. Similarly, catch was low at several upstream locations including Stations 202, 203, and 164 which are not located along the perimeter of the Pond, rather, adjacent to islands.

136

Final Report PBAPS Thermal Study It is difficult to ascertain whether Chesapeake Logperch avoided Stations 214, 215, and 161 during summer because of elevated water temperatures or if their preferred habitat was not present, since so little is known about the life history of this species. In any case, the elevated water temperatures observed during July and August at these stations likely would result in this species avoiding the shallow shoreline habitats near these stations (Table 7-12). The highest water temperature at which Chesapeake Logperch was collected (n=4) during this study was 33.9°C at Station 217 in 2011. The shallow shoreline habitat analysis in Section 5.2 determined that approximately 12 acres of shallow shoreline was present within this section of the Pond from the end of PBAPS discharge canal to Station 215. Much of this habitat is in the immediate vicinity of Burkins Run, with limited shallow shoreline areas downstream of Station 215. It is not known, but unlikely, that substantial numbers of Chesapeake Logperch inhabit Burkins Run as it is a fairly small tributary to the Pond.

A habitat mapping study related to water level fluctuation was completed within the Conowingo Pond during 2010 (URS 2011 ). This study evaluated shoreline sediment class and location of SAV. Several of the locations within the Pond that had the highest catch rates of Chesapeake Logperch were in locations with fairly large areas of shallow shoreline habitat with either sand or gravel sediment present. For example, electrofishing Stations 165 and 217 are in areas with fairly large amounts of shallow habitat adjacent to shoreline. Both these areas have deposits of sediment with a mix of gravel and/or sand as well as fairly substantial beds of SAV (Hydrilla sp.). Electrofishing Station 187 has a smaller area of shallow shoreline habitat with gravel sediment present, but minimal SAV. The collection locations with the lowest catch of Chesapeake Logperch were within areas that had limited shallow shoreline habitat that was composed mostly of bedrock with minimal gravel or sand deposits present. These include electrofishing Stations 189, 190, and 216 and seine Stations 202 and 203. But, several of these stations, with the exception of Stations 189 and 190, were also more distant from tributaries known to be inhabited by Chesapeake Logperch than stations with greater catches of the species. Electrofishing Stations 189 and 190 were in close proximity to Michaels Run, known to be populated by Chesapeake Logperch. Catch was low at the stations closest to the end of the discharge canal (these include seine Stations 214 and 215, and electrofishing Station 161) that experience the highest elevated water temperatures. Shallow shoreline areas were present at these locations with sediment composed of gravel.

An entrainment study completed in 2012 (Normandeau 2013c) at PBAPS characterized the fish assemblage being entrained through the cooling water system. No Chesapeake Logperch were collected during this study. Historic icthyoplankton surveys were completed in Conowingo Pond in relation to the PBAPS intake structure during 1975 and 1976 (Anjard 1975, 1976, 1977). Few larval Chesapeake Logperch were collected in this study. Based on these prior studies, as well as the present study, it is likely that most Chesapeake Logperch spawning occurs in the tributaries and tributary mouths and not in Conowingo Pond proper. Additionally, the length-frequency data for this species shows that few individuals less than 50 mm in length were collected within the Pond from 2010 through 2013 (Figure 5-83 through Figure 5-86) and mean length of Chesapeake Logperch was around 70 mm (Table 5-96 through Table 5-99). In Wisconsin young Logperch ranged between 56-69 mm in length at the end of the first growing 137

Final Report PBAPS Thermal Study season (Lutterbie 1979). Collection of few small individuals also suggests that abundance of Chesapeake Log perch young of the year is low within the Pond.

It is probable that most Chesapeake Log perch spawn in the lower sections and near the mouths of some tributaries to Conowingo Pond in the spring and move into the Pond during summer and fall for feeding and to utilize various preferred habitats. The low numbers collected at shallow shoreline sampling stations directly influenced by the PBAPS thermal discharge may indicate lack of suitable Chesapeake Logperch habitat at these locations. But, the high water temperatures in July and August would still preclude the presence of most Chesapeake Logperch from these locations despite close proximity to potentially suitable stream habitat.

Conclusions

  • A diverse fish community of over 50 species exists in the Pond;
  • CPUEs among species and between stations were variable due to differences in year class strength (i.e. large numbers of young of year of a species being collected at a particular location during given month), habitat preferences, and the constantly changing multitude of environmental variables they experience;
  • Metrics used to describe fish community structure show no clear differences in the fish community between thermally influenced and non-thermally influenced;
  • Avoidance by selected species was observed at Stations 161/214 and 215 at high water temperatures, mostly during July. This was observed in total richness, RIS richness, diversity, and evenness values; Attraction of fishes to Station 161 was observed during January through March;
  • Differences in metric values were not attributable to the proximity of the individual station to the end of the discharge canal, except for the limited avoidance observed in July;
  • Gizzard Shad relative abundance in the Pond was high for most years of the study; however, it is unlikely that the population is dependent on the PBAPS thermal plume or has grown markedly because of the it;
  • Chesapeake Logperch is a threatened species in Pennsylvania that likely avoids areas of potentially suitable habitat during the summer in locations directly downstream from PBAPS;
  • Species richness, diversity, and evenness values observed over the course of study indicate seasonality at all stations with community heterogeneity being similar regardless of location within the Pond;
  • Similar fish assemblages were present at non-thermal and thermal stations with no loss of trophic structure.

138

Final Report PBAPS Thermal Study Table 5-50. Square root transformed mean and median CPUE (no./0.5hr) for all boat electrofishing stations, April to October 2010-2013.

Station Mean Median Total Samples st187 16.9 13 25 st164 16.7 15 25 st165 13.8 13a 25 st161 21.1 17 25 st189 15.4 13b 25 st190 19.3 16 25 st217 26.2 21ab 19 Kruskal-Wallis test, p=0.037, values followed by same letter were significantly different.

Table 5-51. Mean and median species richness for all boat electrofishing stations, April to October 2010-2013.

Station Mean Median Total Samples st187 15.7 16cdf 25 st164 12.2 12ac 25 8

st165 13.4 14 25 st161 12.6 14ef 25 st189 13.7 14h 25 st190 12.3 12bd 25 abegh st217 16.6 16 19 Kruskal-Wallis test, p<0.001, values followed by same letter were significantly different.

139

Final Report PBAPS Thermal Study Table 5-52. Mean and median RIS richness for all boat electrofishing stations, April to October 2010-2013.

Station Mean Median Total Samples abc st187 8.0 9 25 be st164 6.6 7 25 st165 6.6 -,cr 25 st161 6.6 rd 25 st189 7.2 7 25 st190 7.3 7 25 st217 8.1 gdef 19 Kruskal-Wallis test, p<0.001, values followed by same letter were significantly different.

Table 5-53. Mean and median Shannon diversity values for all boat electrofishing stations, April to October 2010-2013.

Station Mean Median Total Samples st187 2.9 3.2abcd 25 st164 2.4 2.7 25 st165 2.7 2.9e 25 st161 2.1 2. 3aef 25 st189 2.7 2.9f 25 st190 2.4 2.7b 25 st217 2.3 2.Sd 19 Kruskal-Wallis test, p<0.001, values followed by same letter were significantly different.

140

Final Report PBAPS Thermal Study Table 5-54. Mean and median evenness for all boat electrofishing stations, April to October 2010-2013.

Station Mean Median Total Samples st187 0.74 0.80ac 25 st164 0.68 0.75 25 st165 0.74 0.79b 25 st161 0.58 0.71c 25 st189 0.71 0.78d 25 st190 0.67 0.71 25 st217 0.56 0.62abd 19 Kruskal-Wallis test, p=0.001, values followed by same letter were significantly different.

80 70 60 w so D. 40 u

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st187 st164 st165 st161 st189 st190 st217 Figure 5-42. Box plot of square root transformed CPUE (no./0.5hr) for all electrofishing stations, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across

=

the box median value, vertical lines extending from the box =highest and lowest values, circle =mean, and asterisk = outlier) 141

Final Report PBAPS Thermal Study 25 20 VI VI GI c 0

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10 st187 st164 st165 st161 st189 st190 st217 Figure 5-43. Box plot of species richness for all boat electrofishing stations, April to October 2010-2013. (boxes= interquartile range containing 50% of the values, the line across the box= median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk =

outlier) 11 10 9

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st187 st164 st165 st161 st189 st190 st217 Figure 5-44. Box plot of RIS richness for all boat electrofishing stations, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) 142

Final Report PBAPS Thermal Study 4

3 0

0 0

0 1

st187 st164 st165 st161 st189 st190 st217 Figure 5-45. Box plot of Shannon diversity values for all boat electrofishing stations, April to October 2010-2013. (boxes= interquartile range containing 50% of the values, the line across the box=

median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) 0.9 0.8 0.7 0

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st187 st164 st165 st161 st189 st190 st217 Figure 5-46. Box plot of evenness values for all boat electrofishing stations, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk =

outlier) 143

Final Report PBAPS Thermal Study 80 70 60 w 50

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interquartile range, line across box = median value, and vertical lines extending from the box = highest and lowest values) 25 20

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5 Figure 5-48. Box plot of species richness by month for all boat electrofishing stations, April to October 2010-2013. (4 =April, 5 =May, 6 =June, etc.) (boxes= interquartile range, line across box

= median value, and vertical lines extending from the box= highest and lowest values) 144

Final Report PBAPS Thermal Study 11 10 9 I~

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=median value, and vertical lines extending from the box= highest and lowest values)

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Figure 5-50. Box plot of Shannon diversity by month for all boat electrofishing stations, April to October 2010-2013. (4 =April, 5 = May, 6 =June, etc.) (boxes= interquartile range, line across box

=median value, and vertical lines extending from the box= highest and lowest values) 145

Final Report PBAPS Thermal Study 1.0

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Figure 5-51. Box plot of evenness by month for all boat electrofishing stations, April to October 2010-2013. (4 =April, 5 =May, 6 =June, etc.) (boxes= interquartile range, line across box= median value, and vertical lines extending from the box = highest and lowest values) 146

Final Report PBAPS Thermal Study Table 5-55. Mean electrofishing CPUE (no./0.5hr) by station for Gizzard Shad collected in Conowingo Pond, April to October 2010-2013.

Station April May June July August September October st187 6.3 4.0 7.7 424.3 35.8 25.3 50.S st164 3.7 17.0 3.0 102.0 658.8 222.0 17.8 st165 19.3 11.7 2.7 63.0 21.S 3.8 15.5 st161 601.0 351.0 1.7 67.0 525.3 527.5 25.5 st189 8.7 25.0 0.7 515.5 272.5 26.0 7.0 st190 4.7 33.3 4.0 125.5 273.5 18.3 9.5 st217 24.0 206.5 9.0 441.7 696.7 37.3 198.3 Table 5-56. Mean electrofishing CPUE (no./0.5hr) by station for Spotfin Shiner collected in Conowingo Pond, April to October 2010-2013.

Station April May June July August September October st187 0.0 1.7 31.7 155.3 7.0 13.3 8.8 st164 1.0 9.3 43.0 20.0 15.3 8.3 12.0 st165 0.3 1.0 3.7 3.5 3.8 1.8 2.0 st161 4.0 39.3 32.3 4.3 8.0 4.8 13.5 st189 2.7 18.3 29.3 8.8 6.8 6.0 10.5 st190 3.0 14.7 17.0 12.0 11.3 5.3 3.8 st217 0.0 4.0 2.7 7.3 12.3 2.0 5.3 Table 5-57. Mean electrofishing CPUE (no./0.5hr) by station for Bluntnose Minnow collected in Conowingo Pond, April to October 2010-2013.

Station April May June July August September October st187 7.7 9.7 11.3 3.5 17.3 15.3 7.8 st164 3.0 12.7 2.3 8.0 0.5 3.3 6.8 st165 2.3 6.3 3.0 1.0 1.8 1.8 5.3 st161 8.7 3.7 6.0 8.3 13.3 5.0 2.5 st189 10.3 13.3 6.3 2.0 4.8 2.3 7.3

- - -- - - st190 ------ 11.3 32.0 14.0 5.0 3.3 3.8 7.3 - ---- ---- - - --

st217 13.0 8.0 1.7 1.0 1.7 1.0 11.3 147

Final Report PBAPS Thermal Study Table 5-58. Mean electrofishing CPUE (no./0.5hr) by station for Channel Catfish collected in Conowingo Pond, April to October 2010-2013.

Station April May June July August September October st187 14.7 14.7 21.7 17.0 18.8 23.5 17.3 st164 6.0 11.3 17.3 21.8 35.5 23.0 14.3 st165 12.0 13.0 19.7 22.0 27.5 25.3 26.3 st161 4.3 19.3 30.3 35.5 17.8 11.8 22.3 st189 11.3 30.3 11.3 10.3 10.3 19.3 25.8 st190 17.3 12.3 14.7 16.8 29.0 25.3 23.5 st217 31.5 20.0 18.0 12.7 27.7 16.7 19.7 Table 5-59. Mean electrofishing CPUE (no./0.5hr) by station for Bluegill collected in Conowingo Pond, April to October 2010-2013.

Station April May June July August September October st187 1.0 3.0 3.3 3.3 27.5 51.5 32.5 st164 7.3 11.0 13.7 11.0 14.0 40.8 34.8 st165 3.3 15.0 10.0 6.3 33.3 27.5 74.0 st161 30.7 20.3 15.3 5.0 36.3 40.8 25.5 st189 20.0 22.0 20.3 15.8 32.8 37.8 54.5 st190 26.3 48.0 31.3 16.3 107.3 298.8 111.5 st217 23.0 115.5 62.3 41.3 975.7 550.3 163.3 Table 5-60. Mean electrofishing CPUE (no./0.5hr) by station for Smallmouth Bass collected in Conowingo Pond, April to October 2010-2013.

Station April May June July August September October st187 7.0 3.3 13.7 10.5 8.5 6.5 15.3 st164 14.0 21.0 7.7 7.8 7.3 30.3 52.5 st165 5.0 14.3 9.0 10.3 6.8 17.0 19.3 st161 3.7 5.7 17.3 7.3 9.5 21.0 24.3 st189 3.3 2.3 6.0 5.5 5.3 3.5 4.5 st190 3.3 3.7 6.7 22.0 5.5 9.8 8.5 st217 1.5 3.5 9.7 23.7 9.0 8.3 6.7 148

Final Report PBAPS Thermal Study Table 5-61. Mean electrofishing CPUE (no./0.5hr) by station for Largemouth Bass collected in Conowingo Pond, April to October 2010-2013.

Station April May June July August September October st187 0.3 0.0 0.7 2.0 1.8 1.5 1.0 st164 3.7 2.0 1.0 0.0 0.0 0.5 0.3 st165 0.7 0.3 0.0 0.3 0.0 0.0 0.3 st161 2.3 0.0 0.0 0.0 0.0 0.3 2.5 st189 2.0 0.7 1.3 1.0 2.5 4.0 3.5 st190 2.0 0.7 0.7 0.8 0.8 3.5 12.3 st217 3.0 5.0 2.7 2.3 5.3 19.0 10.3 Table 5-62. Mean electrofishing CPUE (no./0.5hr) by station for Chesapeake Logperch collected in Conowingo Pond, April to October 2010-2013.

Station April May June July August September October st187 0.0 0.3 0.3 3.5 6.5 12.5 6.5 st164 0.0 0.0 0.0 0.3 0.0 1.3 2.0 st165 0.0 0.3 0.7 4.5 7.5 9.5 8.0 st161 0.3 0.3 0.7 0.0 0.3 1.5 2.3 st189 0.0 0.0 0.3 0.0 0.5 1.8 0.3 st190 0.0 1.3 1.0 3.0 2.5 5.3 1.8 st217 1.5 2.0 3.0 7.7 16.3 17.3 2.7 Table 5-63. Mean electrofishing CPUE (no./0.5hr) by station for Walleye collected in Conowingo Pond, April to October 2010-2013.

Station April May June July August September October st187 3.3 0.7 1.3 2.0 5.5 2.3 9.0 st164 1.7 0.0 0.3 0.0 0.8 2.5 10.0 st165 1.7 0.7 0.0 0.0 0.5 1.0 10.3 st161 1.0 1.3 0.0 0.0 0.3 1.0 13.5 st189 2.3 0.7 0.0 0.0 0.0 0.8 6.5 st190 7.0 0.0 0.0 0.0 0.0 0.5 3.0


st217 0.0 0.0 0.0 0.0 0.3 1.0 3.3 - - ---- --

149

Final Report PBAPS Thermal Study Table 5-64. Square root transformed mean CPUE (no./0.5hr) for all boat electrofishing stations, January- March 2011-2013.

Station January February March st187 8 6 13 st164 30 29 11 st165 13 6 8 st161 12 11 16 st189 9 33 8 st190 12 9 17 st217 8 6 12 Table 5-65. Species richness for all boat electrofishing stations, January- March 2011-2013.

Station January February March st187 6 6 10 st164 8 6 7 st165 8 5 4 st161 13 13 15 st189 9 8 13 st190 10 9 10 st217 7 4 7 Table 5-66. RIS ~ichness for all boat electrofishing stations, January- March 2011-2013.

Station January February March st187 3 2 4 st164 4 3 4 st165 3 2 2 st161 6 7 6 st189 6 3 7 st190 5 3 6 st217 2 2 4 150

Final Report PBAPS Thermal Study Table 5-67. Shannon diversity values for all boat electrofishing stations, January- March 2011-2013.

Station January February March st187 1.69 1.72 1.83 st164 0.97 0.87 0.76 st165 1.65 1.18 0.32 st161 2.67 2.77 2.62 st189 2.24 0.64 2.74 st190 1.54 1.46 0.98 st217 1.60 0.63 0.81 Table 5-68. Evenness for all boat electrofishing stations, January- March 2011-2013.

Station January February March st187 0.65 0.66 0.55 st164 0.30 0.34 0.27 st165 0.68 0.68 0.16 st161 0.73 0.73 0.67 st189 0.70 0.21 0.74 st190 0.46 0.47 0.30 st217 0.57 0.32 0.29 Table 5-69. Mean CPUE for Gizzard Shad, January-March 2011-2013.

Station January February March st187 0 0 0 st164 11 0 7 st165 10.5 0 1 st161 1 29.5 100 st189 13 1.5 6 st190 10.5 2.5 8 st217 0 0 3 151

Final Report PBAPS Thermal Study Table 5-70. Square root transformed mean and median CPUE (no/collection) for seine stations, April to October 2010-2013.

Station Mean Median Total Number st202 6.1 5.3 24 st203 5.3 5.4a 24 st220 7.4 7.3a 24 st221 6.3 5.3 24 st208 5.7 5.1 24 st214 6.5 6.2 24 st215 6.0 5.6 24 Kruskal-Wallis test, p=0.1, values followed by same letter were significantly different.

Table 5-71. Mean and median species richness for seine stations, April to October 2010-2013.

Station Mean Median Total Number st202 5.4 5 24 st203 5.3 5 24 st220 6.5 5.5a 24 st221 5.6 5 24 st208 5.6 5 24 st214 5.1 5 24 st215 3.7 4a 24 Kruskal-Wallis test, p=0.05, values followed by same letter were significantly different.

152

Final Report PBAPS Thermal Study Table 5-72. Mean and median RIS richness for seine stations, April to October 2010-2013.

Station Mean Median Total Number st202 2.4 2 24 st203 2.3 2 24 st220 3.4 3 24 st221 2.5 2 24 st208 2.8 3 24 st214 2.8 3 24 st215 2.7 3 24 Kruskal-Wallis test, p>0.2, no significant differences between stations.

Table 5-73. Mean and median Shannon diversity for seine stations, April to October 2010-2013.

Station Mean Median Total Number st202 1.6 1.5 24 st203 1.6 1.7 24 st220 1.6 1.6 24 st221 1.7 1.6a 24 st208 1.7 1.6 24 st214 1.4 1.5 24 st215 1.1 1.1a 24 Kruskal-Wallis test, p=0.09, values followed by same letterwere significantly different.

153

Final Report PBAPS Thermal Study Table 5-74. Mean and median evenness for seine stations, April to October 2010-2013.

Station Mean Median Total Number st202 0.7 0.7 24 st203 0.7 0.8 24 st220 0.6 0.7 24 st221 0.7 0.7 24 st208 0.7 0.8 24 st214 0.6 0.7 24 st215 0.6 0.7 24 Kruskal-Wallis test p=0.16, no significant differences between stations.

16 14 12 w 10

  • e; 8

> 0 0 6 0 4

2 st202 st203 st220 st221 st208 st214 st215 Figure 5-52. Box plot of square root transformed CPUE (no./collection) by station for seine collections, April to October 2010-2013.(boxes =interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) 154

Final Report PBAPS Thermal Study 14 12 10 81

~ 8 en 0

  • ~ 6 0 0 i 0 0 4

2 st202 st203 st220 st221 st208 st214 st215 Figure 5-53. Box plot of fish species richness (no./collection) by station for seine collections, April to October 2010-2013. (boxes= interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) 7 6

5 en en I!!

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st202 st203 st220 st221 st208 st214 st215 Figure 5-54. Box plot of RIS richness (no./collection) by station for seine collections, April to October 2010-2013. (boxes= interquartile range containing 50% of the values, the line across the box =

median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) 155

Final Report PBAPS Thermal Study 3.0 2.5 2.0 0

0 1.0 0.5 0.0 st202 st203 st220 st221 st208 st214 st215 Figure 5-55. Box plot of Shannon diversity values by station for each monthly seine collection, April to October 2010-2013. (boxes= interquartile range containing 50% of the values, the line across the box = median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) 1.0 0.8 0 0 0

0 0

acu 0.6 0 c

c cu

~

0.4 0.2 **

0.0 st202 st203 st220 st221 st208 st214 st215 Figure 5-56. Box plot of evenness values by station for each monthly seine collection, April to October 2010-2013. (boxes = interquartile range containing 50% of the values, the line across the box =

median value, vertical lines extending from the box = highest and lowest values, circle = mean, and asterisk = outlier) 156

Final Report PBAPS Thermal Study Table 5-75. Mean seine CPUE (no./collection) by station for Spotfin Shiner collected in Conowingo Pond, April to October 2010-2013.

Station Af;!ril Ma:i'. June Jul:i'. August Sef:!tember October st202 3.7 4.7 13.0 7.5 14.0 11.5 3.8 st203 6.0 5.7 7.3 5.3 4.8 13.3 3.5 st220 31.7 7.3 18.7 16.3 29.5 38.5 44.8 st221 13.3 5.0 7.0 6.8 8.5 1.8 3.0 st208 2.3 6.3 5.7 47.5 6.5 9.0 25.5 st214 11.7 9.3 19.7 15.5 13.3 17.3 9.5 st215 13.3 11.3 15.7 36.5 31.0 21.5 16.8 Table 5-76. Mean seine CPUE (no./0.5hr) by station for Bluntnose Minnow collected in Conowingo Pond, April to October 2010-2013.

Station Af;!ril Ma:i'. June Jul:i'. August Sef:!tember October st202 11.7 6.7 6.0 9.5 7.5 4.3 2.8 st203 3.0 10.0 12.3 13.3 22.3 2.5 3.3 st208 4.7 8.3 6.3 10.0 13.8 5.5 2.0 st220 18.7 7.3 11.3 12.5 14.5 2.5 14.3 st221 3.3 3.3 3.0 1.5 6.8 31.5 0.3 st214 16.7 18.0 9.7 17.0 28.3 4.8 6.8 st215 10.7 5.7 6.0 10.0 13.5 2.3 5.8 Table 5-77. Mean seine CPUE (no./collection) by station for Bluegill collected in Conowingo Pond, April to October 2010-2013.

Station Af:!ril Ma:i'. June Jul:i'. August Se~tember October st202 0.0 0.0 0.0 0.3 17.5 68.5 1.3 st203 0.0 0.3 0.0 0.0 6.8 1.0 1.3 st220 0.0 0.0 0.0 0.8 10.3 29.8 4.8 st221 0.3 0.0 0.0 0.3 0.3 1.0 0.0 st208 0.0 0.0 0.0 2.3 3.5 2.0 3.5 st214 0.7 0.3 1.0 1.8 2.5 4.8 0.8 st215 0.3 0.0 0.0 7.0 15.3 2.3 2.5 157

Final Report PBAPS Thermal Study Table 5-78. Mean seine CPUE (no./collection) by station for Smallmouth Bass collected in Conowingo Pond, April to October 2010-2013.

Station A~ril Ma~ June Jul~ August Se~tember October st202 0.0 0.0 2.0 1.5 0.5 0.0 0.0 st203 0.0 0.0 1.3 0.5 0.3 0.0 0.0 st220 0.0 0.0 1.0 2.3 1.5 0.3 0.0 st221 0.0 0.0 0.7 0.8 0.5 0.0 0.0 st208 0.0 0.0 0.7 1.5 0.8 0.5 0.0 st214 0.0 0.0 1.0 0.3 0.0 0.0 0.0 st215 0.0 0.0 2.7 1.3 0.8 0.0 0.0 Table 5-79. Mean seine CPUE (no./collection) by station for Chesapeake Logperch collected in Conowingo Pond, April to October 2010-2013.

Station A~ril Ma~ June Jul~ August Se~tember October st202 0.0 0.0 0.0 0.0 0.3 0.0 0.0 st203 0.0 0.0 0.0 0.0 0.0 0.0 0.0 st220 0.0 0.0 0.3 2.3 6.5 0.8 0.3 st221 1.3 0.0 0.0 0.0 0.8 0.0 0.0 st208 0.0 0.7 1.0 0.3 1.8 0.0 0.3 st214 0.0 0.0 0.0 0.0 0.3 0.0 0.0 st215 0.0 0.0 0.0 0.0 0.0 0.3 0.3 158

Final Report PBAPS Thermal Study 16 14 12 w 10 A.

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Figure 5-58. Box plot of species richness by month for all seine stations, April to October 2010-2013. (4=April, S=May, 6=June, etc.) (boxes = interquartile range, line across box = median value, and vertical lines extending from the box= highest and lowest values) 159

Final Report PBAPS Thermal Study 7

6 5 ~

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0 Figure 5-59. Box plot of RIS richness by month for all seine stations, April to October 2010-2013. (4=April, 5=May, 6=June, etc.) (boxes = interquartile range, line across box = median value, and vertical lines extending from the box= highest and lowest values) 3.0 2.5 >-- t-1---- >---

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- - -- - - 0.0 Figure 5-60. Box plot of Shannon diversity values by month for all seine stations, April to October 2010-2013. (4=April, 5=May, 6=June, etc.) (boxes = interquartile range, line across box =

median value, and vertical lines extending from the box= highest and lowest values) 160

Final Report PBAPS Thermal Study 1.0

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~ ~ ~ ~ ~ § Figure 5-61. Box plot of evenness values by month for all seine stations, April to October 2010-2013. (4=April, 5=May, 6=June, etc.) (boxes = interquartile range, line across box= median value, and vertical lines extending from the box = highest and lowest values) 90 - - - -

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0 .. - ~ r 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 Year Figure 5-62. Number of Gizzard Shad passed at Conowingo, Holtwood, Safe Harbor, and York Haven Dam, 1997-2011. Data taken from Exelon's annual Cowowingo Dam fish lift reports.

161

Final Report PBAPS Thermal Study Fish-Water Temperature Observations 1 Fish were collected over a wide range of water temperatures during the course of the four year study. Water temperatures at the time of field collections ranged from 1.5°C (34. 7°F) to 36.6°C (97.9°F). Data presented in this section pertains to boat electrofishing and seine collections completed from April to October, 2010-2013. During the course of field collections instantaneous water temperature measurements were completed at each station. Water temperatures were measured within a few feet of the water surface and these temperatures reflect the entire water column at these shallow shoreline seine and electrofishing stations, as the water is fully mixed with no temperature stratification.

To elucidate the relation of fish occurrence to collection water temperature, the total number of each fish species observed at both non-thermally and thermally influenced stations was tabulated. For this analysis stations are discussed as either non-thermal or thermal based on their location in relation to the PBAPS thermal plume. Stations downstream of the discharge canal that experience elevated water temperatures above ambient water temperature for the entire collection period are considered to be thermally influenced. Stations that are upstream of the PBAPS thermal discharge that experience natural water temperature conditions are considered non-thermal (Figure 5-22 to Figure 5-24; Table 5-12 to Table 5-14). Electrofishing Stations 161, 189, 190, and 217 are considered thermally influenced and Stations 187, 164, and 165 are considered non-thermal. Seine Stations 214 and 215 are considered thermally influenced and Stations 203, 202, 220, 221, and 208 are considered non-thermal. As previously discussed in Section 5.2, Station 208 does experience elevated water temperatures during a portion of the year resulting from thermal plume movement upstream during low flow conditions; however, this station is considered non-thermal because it does not experience a prolonged thermal influence.

Fish occurrence over a range of water temperatures was determined with particular emphasis on water temperatures >25°C (77°F) which represents ambient water temperatures during the warmer period of the year, roughly from June to September. Time series plots of daily mean and instantaneous maximum water temperature for the monitoring stations are provided previously in Figure 5-1 through Figure 5-9 and show the complete temperature history for each station.

Table 5-80 provides the total number of each fish species collected over a range of water temperatures for the non-thermal stations. Maximum water temperature observed at the non-thermal stations was 32°C (89.6°F). Most of the abundant RIS were collected over a wide range of summer water temperatures up to the near maximum ambient water temperature of 32°C.

Table 5-81 provides the total number of each fish species collected over a range of water temperatures for the thermally affected stations. The maximum water temperature observed for 1

Temperature values are provided in both English (Fahrenheit) and metric (Centigrade) units due to the widespread use of metric units in the scientific literature.

162

Final Report PBAPS Thermal Study the thermally affected stations was 36.6°C (97.9°F). Water temperatures ~ 32°C represents water temperatures that were greater than those observed at any of the non-thermal stations.

Ten of the RIS were collected at water temperatures ~ 32°C. The only RIS not collected at elevated water temperatures was Walleye, with few of this species collected at water temperature exceeding 25°C. The highest temperature that Walleye were collected was in the 29-29.9°C (84.2-85.8°F) range for the non-thermal stations (Table 5-80); however, similar to thermal stations, most Walleye were collected at water temperatures s 25°C.

In general, species richness decreased as water temperatures increased above 33°C (91.4°F).

For example, 11 species were collected between temperatures of 33-33.9°C (91.4-93.0°F) and only six species were collected at the highest temperatures between 36-36.9°C (96.8-97.9°F).

Relatively few individuals were collected at the highest water temperatures for most species except Spotfin Shiner. Spotfin Shiner was collected in fairly large numbers for all water temperature ranges up to and including 36-36.9°C. It should be noted that the comparison here is not standardized for effort, that is, fewer samples were collected at the highest water temperatures. However, comparing absolute numbers of individuals for a given species is useful in showing the approximate delineation where most species begin to avoid locations within the Pond because of elevated water temperatures.

Conclusions Fish were collected at a wide range of water temperatures during the course of this study. Fish species distribution and community composition were similar between the non-thermal and thermal stations. Each of the 11 RIS was collected at both the non-thermal and thermally influenced stations. No thermally stressed fish were observed, with fish maintaining normal activity prior to collection and after processing and release. Field observations during this study found no indications that fish (4, 130 individuals, 2010-2013) collected at water temperatures

~32°C (89.6°F), which is the maximum ambient water temperature observed, were experiencing thermal stress.

Few fish were collected at water temperatures greater than 36°C (96.8°F). Water temperatures greater than 36°C (96.8°F) observed during fish surveys occurred only during July at the near-field stations (214, 215, and 161). For the thermally influenced locations, ten of the 11 RIS were collected at elevated water temperatures between 30-33°C (86-91.4 °F) and eight of the 11 RIS were collected at water temperatures between 33-36°C (91.4-96.8°F). Three of the RIS (Walleye, White Sucker, and White Crappie) were not collected at water temperatures between 33-36°C (91.4-96.8°F). Few individuals of these three species were collected at water temperatures >25°C. Twenty-one species of fish were collected at water temperatures that exceeded 33°C (91.4°F).

The next section provides gear-specific CPUE by station for the observed collection water temperatures during July and August, which is a complementary analysis to this section.

163

Final Report PBAPS Thermal Study Table 5-80. Number of each species collected using seine and electrofishing gear across a range of water temperature for non-thermally affected locations within Conowingo Pond, April-October, 2010-2013.

Water tem~rature *c Taxon <25.0 25- 25.9 26- 26.9 27 - 27.9 28- 28.9 29- 29.9 30- 30.9 31 - 31.9 32 - 32.9 Gil2Brd shad 1,645 17 2,353 469 1,256 1,052 24 31 5 Central stoneroller I Common carp 88 9 37 15 2 3 Cutlips minnow River chub I 2 Golden shiner 3 4 Comely shi:Jer 2,976 39 115 27 149 8 17 2 Common shiner I 4 Spottail shiner 491 150 110 38 148 12 42 Swallowtail shiner 5 2 2 I I Spotfin shiner 1,451 156 207 59 238 646 148 224 4 Mimic shiner 6 2 Bluntnose minnow 677 122 249 70 108 33 25 13 Semotilus sp I Creek chub 9 3 Fallf15h 10 5 3 7 I Quillback 37 2 2 59 3 II White sucker 105 7 1 1 2 7 Northern hogsucker 29 3 2 3 13 7 5 7 Shorthead redhorse 217 2 80 3 23 5 28 5 Channe I catfish 855 76 165 52 127 46 80 12 16 Flathead catf1Sh 22 3 7 3 12 2 2 Banded killif1Sh 675 17 47 8 5 Eastern mosquitofish White perch 45 Striped bass x white bass 4 Rock bass 738 24 71 II 71 27 12 4 6 Redbreast sunflSh 8 3 4 Green sunflSh 646 53 91 52 23 47 18 3 2 Pumpkinseed 14 Bluegill 1,444 305 205 110 78 78 26 2 Smallmouth bass 845 26 95 6 71 15 47 6 Largemouth bass 39 3 7 9 3 5 2 White crappie 11 Black crappie 3 Greenside darter 16 4 4 Tessellated darter 171 18 36 15 40 4 9 Banded darter 4 Yellow perch 90 3 3 6 Chesapeake logperch 205 6 23 25 17 22 17 Shield darter 25 4 13 Walleye 185 2 9 4 2 2 Total number 13,799 1,059 3,932 988 2,475 2,015 526 327 39 Total S~cies 40 30 30 23 27 23 22 15 9 164

Final Report PBAPS Thermal Study Table 5-81. Number of each species collected using seine and electrofishing gear across a range of water temperature for thermally affected locations within Conowingo Pond, April-October, 2010-2013.

Water teml!!:rature *c Taxon <25.0 25 - 25.9 26- 26.9 27 - 27.9 28- 28.9 29- 29.9 30 - 30.9 31 - 31.9 32 - 32.9 33 - 33 9 34 - 34,9 35 - 35.9 36- 36.9 American shad I Gizzanl shad 3,446 SI 381 830 3,878 2,8S2 2,362 1,091 1,02S 1,3S4 4 17 3 Central stonerollcr I 4 Rosysidc dace Grass carp Common carp 152 17 6 15 17 17 4 Golden shiter 20 II 12 18 10 10 4 Comely shiter 3,156 40 24 161 120 153 94 28 19 II 3 Spottail shiner 178 I II 48 17 26 7 18 I 2 Swallowtail shiner I Rosyface shiner Spotin shiner S9S 99 SS 209 17S 193 S2 187 128 146 270 121 96 Minic shiner 2 I

--~

Bluntnose minnow 448 24 14 76 47 27 11 38 10 16 16 13 Blacknosc dace I Creek chub 12 3 4 FaOflSh 7 2 2 Quillback 9 6 2 2 White sucker 8 2 Northern hogsucker 4 Shorthead redhorse 159 II 27 6 19 7 12 16 Channe I catfish 802 41 208 83 78 131 61 IS8 89 119 10 S7 Flathead catfish 19 I 6 12 8 8 2 9 2 I 2 Atlantic needlcfish Banded kiDifish 221 38 8 2 White perch 35 17 Striped bass Striped bass "white bass 31 Rock bass 153 9 22 6 10 16 10 4 6 4 Redbreast swtfish 4 2 I Green swtfish 1,221 100 250 230 712 413 91 245 24 36 31 53 Pumpkinseed 10 2 2 I I I Bluegill 4,731 171 386 275 3,006 496 146 13S ISO 30 92 16 7 Smallmouth ban 295 16 73 80 S6 S3 33 169 39 21 6 22 Largemouth bass 214 11 2S 10 10 3 s 2 2 s 3 White crappie 21 2 2 2 Black crappie 4 I Greer1Sidc darter 12 2 2 Tessellated daner 69 3 2 4 Yellow perch 28 Chesapeake logpe n:h 111 3 43 16 17 12 11 22 4 Shield daner II 2 I Walleye 146 s 2 Total nwnbcr 16.342 634 1,578 2,096 8,202 4,451 2,915 2,150 1,513 1,760 438 309 110 Total S!!!:cics 37 25 26 25 25 28 19 25 21 17 II 13 6 165

Final Report PBAPS Thermal Study Temperature-CPUE comparison This section describes fish catch at the electrofishing and seining locations during July and August and the measured water temperature at the time of collection. July and August are the two months of the year associated with the highest collection waters temperatures at both the non-thermal and thermal stations in the Pond (Figure 5-1 through Figure 5-9). Elevated water temperatures can result in species-specific avoidance and, thus, the following discussion evaluates the difference in CPUE and species richness with specific emphasis on the RIS.

For this analysis stations are discussed as either non-thermal or thermal based on their location in relation to the PBAPS thermal plume. Stations downstream of the discharge canal that experience elevated water temperatures above ambient water temperature for the entire collection period are considered to be thermally influenced. Stations that are upstream of the PBAPS thermal discharge that experience natural water temperature conditions are considered non-thermal (Figure 5-22 and Figure 5-23). Electrofishing Stations 161, 189, 190, and 217 are considered thermally influenced and Stations 187, 164, and 165 are considered non-thermal.

Seine Stations 214 and 215 are considered thermal influenced and Stations 203, 202, 220, 221, and 208 are considered non-thermal. As previously discussed in Section 5.2, Station 208 does experience elevated water temperatures during a portion of the year resulting from thermal plume movement upstream during low flow conditions; however, this station is considered non-thermal because it does not experience a prolonged year-round thermal influence.

Electrofishing Table 5-82 through Table 5-84 provide CPUE by species and observed water temperature for the three non-thermal electrofishing stations during July and August, 2010-2013. For Station 187, the most upstream collection location, water temperature varied from 24.2 to 30.9°C (75.6-87.60F). Station 187 generally had high fish diversity during both months with 12 to 20 species observed. Ten of the 11 RIS were present during most of the collections. CPUE at Station 187 was highly variable among months and years of collection. Similarly, for Station 165, 10 RIS were observed during July and August, 2010-2013. Water temperature at this location ranged from 20.3 to 32°C (68.5-89.6°F). Six RIS were collected during most months (Gizzard Shad, Spotfin Shiner, Chesapeake Logperch, Bluegill, Smallmouth Bass, Channel Catfish); while others were collected less frequently. Species richness ranged from 9 to 18 species. For Station 164, collection water temperature ranged from 24.4 to 31°C (75.9-87.8°F). A total of 8 RIS were collected with most of the RIS observed during each collection. Total species richness varied from 8 to 13 species. Most of the observed RIS at this location were collected

--- - - during most months with variable CPUE. Few Walleye or Chesapeake Logerch were collected ----- -

at this location.

Table 5-85 through Table 5-88 provide CPUE by species and observed water temperature for the four thermally affected electrofishing stations during July and August, 2010-2013. Station 161, the location closest to PBAPS, experienced the highest observed water temperatures ranging from 29.2 to 35.2°C (84.6-95.4°F). Species richness ranged from 6 to 14 species.

Greater numbers of species were collected at the lowest water temperatures (n=14 in August 2011, temperature 31.2°C; n=14 in August 2013, temperature 29.2°C) during these two months.

166

Final Report PBAPS Thermal Study Species richness was generally low at water temperatures that exceeded 33°C. Fewer species were observed during July than August for all years with a total of 8 RIS observed. Two RIS, Chesapeake Logperch and Walleye were only observed in August 2013. The other commonly collected RIS had quite variable CPUE. Station 189 observed water temperature range was 27.?°C to 34.2°C (81.9-93.6°F). Total species richness ranged from 8 to 15, with 9 RIS collected. Most the observed RIS were present during each sample month including Gizzard Shad, Spotfin Shiner, Bluntnose Minnow, Channel Catfish, Bluegill, and Smallmouth Bass. No consistent pattern in species richness or CPUE related to collection temperature was observed.

For Station 190, collection temperature ranged from 26.5 to 33.9°C (79.7-93°F). Species richness was similar for most months ranging from 8 to 12 species, although the fewest species were collected at the highest observed water temperature (33.9°C) in July 2011. A total of 8 RIS observed during July and August with CPUE varying widely from month to month and year to year. For example in 2013, 66 Smallmouth Bass were collected in July at water temperature of 31.5 °C and only 13 were collected in August at water temperature of 26.5°C. For the most downstream location (Station 217), water temperature ranged from 26.1 to 33.9°C (79-93°F).

All 11 RIS were observed at least once during July or August. Monthly species richness ranged from 10 to 18 species and was not well correlated to water temperature. CPUE varied widely for the RIS. Smallmouth Bass CPUE was much higher during July (55/ 0.5hr) and August (21/

0.5hr) 2013 compared to most other months. Chesapeake Logperch catch was also higher during August 2013 (28/0.5hr) compared to most other collections. Otherwise, there were no well-defined trends in RIS CPUE among years.

Seine Table 5-89 through Table 5-93 provide CPUE by species and observed water temperature for the five non-thermal seining stations during July and August, 2010-2013. For Stations 202 and 203, the most upstream stations which are both adjacent to islands, water temperature varied from 25.3 to 28.9°C (77.5-84°F). Station 202 species richness ranged from 4 to 8 species and Station 203 species richness ranged from 2 to 10 species. Seven of the 11 RIS were present during at least one collection at these two stations. CPUE was highly variable among months and years of collection with Spotfin and Spottail Shiner present in all collections. For Station 220, collection water temperature ranged from 24.8 to 30.8°C (76.6-87.4°F). Species richness varied from 2 to 14 species with highly variable CPUE. A total of 6 RIS were collected with only Spotfin Shiner and Smallmouth Bass observed during each collection. Spotfin Shiner CPUE was generally high, ranging from 11 to 50 individuals per collection. At Station 221, species richness ranged from 4 to 13 species with .8 RIS observed. Water temperature at this location ranged from 21 .2 to 31.2 °C (70.2-88.2°F). The Spotfin Shiner was the only RIS collected in every month at this station; while the other RIS were collected less frequently. For the most downstream location (Station 208) water temperature ranged from 26.5 to 31. 7°C (79. 7-89.1°F).

A total of 7 RIS were collected at this station with species richness ranging from 3 to 13 species.

Spotfin Shiner had the highest CPUE and was collected during all months. Most other species were collected infrequently with few individuals in each collection.

Table 5-94 and Table 5-95 provide CPUE by species and observed water temperature for the two thermal seining stations during July and August, 2010-2013. Station 214, the location 167

Final Report PBAPS Thermal Study closest to PBAPS, experienced the highest observed water temperatures, ranging from 31.4 to 36.6°C (88.5-97.9°F). Species richness ranged from 1 to 7 species. Species richness was low at water temperatures that exceeded 34°C (93.2°F). Only Spotfin Shiner was collected at the highest observed water temperature (36.6°C). Fewer species were observed during July compared to August for all years. A total of 8 RIS were observed across all years. CPUE was low for all species except Spotfin Shiner. Station 215 observed water temperature range was 30.3°C to 36.2°C (86.5-97.2°F). Species richness ranged from 1 to 7, with 7 RIS collected.

Only Spotfin Shiner was collected during each month with CPUE for this species being high for most months. Similar to Station 214, fewer species were collected at water temperatures greater than 34°C.

Discussion The observations of fish community composition at the electrofishing stations during July and August indicated widely varying CPUE for most species and variation in species richness at both thermally affected and non-thermally affected stations. Stations 187 and 165 (non-thermal) and 217 (thermal) had the greatest observed species richness among the electrofishing stations.

Gizzard Shad CPUE was extremely variable and tended to comprise a large percentage of the overall catch for most locations. This is typical for this species which can be collected in large numbers due to presence of a large school within a sample reach. Other RIS were collected frequently at most electrofishing stations during these months including Bluegill, Smallmouth Bass, Channel Catfish, and Spotfin Shiner. Chesapeake Logperch abundance was highest at Stations 187 and 217 with CPUE typically lower at the other locations. This species was collected during each month for all years at these two locations. Several RIS had low CPUE and occurred infrequently during these months including Walleye, White Sucker, and White Crappie. Few White Sucker or White Crappie were collected during the entire four year study regardless of collection month. Relative abundance of these two species is low in the Pond.

CPUE and species richness for most fish species was not related to collection temperature except at Station 161 where fewer species were collected at the highest water temperatures. A pattern of avoidance was observed at Station 161 at the highest water temperatures (>33 °C) with the lowest species richness (n =6) in July and August 2010. Species richness during these periods was lower than the lowest values observed at all other non-thermal or thermal stations.

CPUE at this station was also low at the highest water temperatures for the limited number of species observed in July, 2011 and 2013. Figure 5-47, provided previously in Section 5 (Fish Metrics and CPUE) illu_strates month to month variation in species richness among station and shows a clear depression in richness during July and in some years August at Station 161. No clear pattern of avoidance at the other thermally affected locations was observed.

The observations of fish community composition at the seining stations during July and August indicated widely varying CPUE for most species and variation in species richness among locations. Stations 220 and 221 (non-thermal) had the greatest observed species richness among the seine stations. The highest observed collection water temperatures were observed at Stations 214 and 215 which are both thermally affected. At the highest water temperatures 168

Final Report PBAPS Thermal Study few species were present and CPUE was low for the species that were present with the exception of Spotfin Shiner. Spotfin Shiner CPUE was high for some months even at the highest observed water temperatures. Species richness was low at both thermally affected stations with few species observed when water temperature exceeded 34°C, an indication that most fishes avoided these areas. Fish avoidance at Stations 214 and 215 occurred during most July and August collections with the exception of a few collections where species richness was comparable to the non-thermal stations.

Wide variation in CPUE among species and months was observed among the seine stations.

Spotfin Shiner had the highest CPUE and was the most commonly collected species among the stations. This species was present at the highest water temperatures, an indication that this species may be more tolerant to higher water temperatures than most other species in the Pond. Most other fishes were collected sporadically with quite variable CPUE. For example, White Sucker CPUE was low for most months and years with exception of Station 221where29 individuals were collected in August 2013, more than the combined total for all other stations and months.

In 2013 more species were observed, at both thermal and non-thermal locations for both electrofishing and seining, as compared to previous years' collections in July and August. This general observation was most evident in the electrofishing catch with species richness for the seine collections being more variable. The greater species richness may be related to higher River flows and lower overall water temperatures observed in July and August 2013 compared to previous years. Species preferring these cooler conditions combined with higher overall flows may have moved farther downstream into the mid- and lower-Pond where the field collections occurred. In contrast, during 2010 fewer species were observed at most electrofishing locations compared to the other years.

Besides year to year variation, station differences related to physical habitat and location in the Pond also determine species distribution and occurrence at a given station. The upstream non-thermal stations at the upper part of the Pond are influenced more by flows from Holtwood Dam (free-flowing riverine environment) and the lower portions of the Pond are more characteristic of impoundment, with little direct influence from Holtwood Dam releases. Thus the stations are located on a gradient of influence from upstream to downstream that likely, in part, shapes the characteristics of the fish community present at a given location.

Observed collection water temperature is a useful means to determine the instantaneous water temperature-fish occurrence relationship. However, the recent water temperature history at a

- -- -- station is also likely to be quite important in determining the fish community present at a given -- - -

location in the Pond. Instantaneous water temperature, although related, does not account for the days or weeks leading up to the collection. Water temperatures at a given location, particularly at the thermally influenced stations, could have been quite different from the observed instantaneous water temperatures based on the highly variable nature of River flow and ambient water temperature in the Pond. As discussed previously in Section 3.4, flow and ambient water temperature are strong predictors of the spatial characteristics of the PBAPS thermal plume.

169

Final Report PBAPS Thermal Study Table 5-82. CPUE (number/O.Shr) and water temperature for fishes collected with a boat electrofisher at Station 187, July and August 2010-2013.

2010 2011 2012 2013 July August Ju~ August Ju~ Au~ust Ju~ August Collection water temperature ( C)0 28.5 26.8 29.2 26 28.1 26.I 30.9 24.2 Gilzard shad 6 21 1,051 34 623 39 17 49 Common carp 5 6 2 10 12 3 5 Golden shiner 2 Comely shiner 7 3 4 9 20 15 2 20 SJX>ttail shiner 11 22 Spotfin shiner 12 9 562 12 5 47 5 Bluntnose minnow 5 2 60 2 4 7 Quillback 2 White sucker 2 1 Northern hogsucker 3 2 I Shorthead redhorse 3 10 18 19 26 27 Channel catfish 13 7 9 30 20 15 26 23 Flathead catfish 2 4 I White perch 3 Rock bass 19 II 12 8 IO 7 10 9 Green sunfJSh 2 2 8 3 4 5 Pumpkinseed Bluegill 2 15 2 72 2 7 7 16 Smallmouth bass 11 1 10 11 5 4 16 18 Largemouth bass 1 1 2 2 3 5 1 Greenside darter Tessellated darter 6 Yellow perch 6 4 Chesapeake logperch 3 7 1 11 4 2 6 6 Shield darter 2 Walleye 1 2 2 1 3 4 2 15 Tota!CPUE 86 107 1,665 306 725 133 185 216 Total s~cies 12 17 16 20 16 16 18 19 170

Final Report PBAPS Thermal Study Table 5-83. CPUE (number/O.Shr) and water temperature for fishes collected with a boat electrofisher at Station 164, July and August 2010-2013.

2010 20I I 20I2 2013 Ju~ August Ju~ August Ju~ Au~t Ju~ A~ust Collection water temperature ( C) 0 28.5 27 3I 26.3 28.2 26.5 30.4 24.4 Gizzard shad 20 451 31 2,061 354 108 3 15 Common carp 2 I Comely shiner 5 5 27 53 I8 5 I2 Spottail shiner 4 I 3 Spotfin shiner 21 16 17 40 30 39 4 Bluntnose minnow 1 3 1 2 1 Fallfish I Northern hogsucker Shorthead redhorse Channel catfish 26 24 12 18 22 7 27 34 Flathead catfJSh 3 I I 2 2 3 Rock bass 2 2 5 8 2 3 Redbreast sunfJSh 3 Green sunfJSh 5 12 3 3I 3 4 6 II Bluegill 3 10 1 15 29 6 11 25 Smallmouth bass 10 6 8 6 5 9 16 Tessellated darter Yellow perch Chesapeake logperch 1 Walleye 3 Tota!CPUE 96 522 73 2,208 5I8 154 108 I29 Total species IO 9 8 II I3 11 II 13 171

Final Report PBAPS Thermal Study Table 5-84. CPUE (number/0.5hr) and water temperature for fishes collected with a boat electrofisher at Station 165, July and August 2010-2013.

2010 2011 2012 2013 July August July August Ju!l August Ju!l August Collection water temperature ("C) 28 29 32 27 28.8 26.2 30.6 20.3 Gi7.zard shad 35 5 16 210 57 2 13 Common carp 5 3 3 2 Comely shiner 9 2 22 42 7 6 9 Spottail shiner 27 6 Swallowtail shiner l Spotfin shiner 3 9 4 5 2 6 1 Mimic shiner 2 Bluntnose minnow 1 3 4 1 1 Quillback Northern hogsucker Shorthead redhorse l Channel catfish 26 37 16 28 19 17 27 28 Flathead catfJSh 2 2 2 2 White perch l Rock bass 22 11 6 9 5 7 4 Redbreast sunfJSh Green sunfJSh 44 2 25 4 25 8 18 Bluegill 6 51 2 54 9 14 8 14 Smallmouth bass 16 3 1 3 6 5 18 16 Largemouth bass 1 White crappie 1 Greenside darter 2 Tessellated darter Banded darter Chesapeake logperch 8 8 17 1 10 4 Shield darter 10 l Walleye 2 Tota!CPUE 138 171 39 228 311 136 88 117 Total SE:cies 16 12 9 18 14 9 11 16 172

Final Report PBAPS Thermal Study Table 5-85. CPUE (number/0.5hr) and water temperature for fishes collected with a boat electrofisher at Station 161, July and August 2010-2013.

2010 2011 2012 2013 Ju~ Au~t Ju~ A~ust Ju~ August Ju~ A~ust Collection water tem~rature ("C) 33.5 35 35.2 31.2 33.9 32.1 35.2 29.2 Gilzard shad 249 17 1,050 19 1,012 22 Common carp I 2 Golden shiner Comely shiner 9 74 Spottail shiner 13 3 Rosyface shiner Spotfin shiner 3 4 3 17 33 46 7 10 Bluntnose minnow 3 4 1 4 Quillback Shorthead redhorse 1 2 Channel catfish 10 13 17 32 89 15 26 11 Flathead catfJSh 1 Redbreast sunfJSh Green sunfJSh 12 8 97 19 14 30 29 Pumpkinseed Bluegill 1 1 2 5 IO 88 7 51 Smallmouth bass 1 1 4 8 9 20 24 Greenside darter Chesapeake logperch 1 Walleye 1 TotalCPUE 265 48 33 1,227 183 1,196 93 235 Total species 6 6 7 14 8 IO 8 14 173

Final Report PBAPS Thermal Study Table 5-86. CPUE (number/O.Shr) and water temperature for fishes collected with a boat electrofisher at Station 189, July and August 2010-2013.

2010 2011 2012 2013 Ju~ Au~ust Ju~ Au~ust July August Ju~ A~ust Collection water temperature ("C) 30.8 30. l 34.2 28.8 31 29.8 32.7 27.7 Gizz.anl shad 2,054 18 754 3 313 5 5 Common carp 4 3 2 Golden shiner 3 Comely shiner 47 4 5 2 10 Spottail shiner 15 Spotfin shiner 3 2 12 19 1 3 19 5 Mimic shiner 1 Bluntnose minnow 2 1 3 1 1 6 11 Shorthead redhorse 2 Channel catfish 1 8 10 11 8 6 22 16 Flathead catfJSh 3 5 Rock bass 2 2 4 4 3 Redbreast sunfJSh Green sunfJSh 2 17 3 33 6 8 5 37 Bluegill 14 18 8 50 11 15 30 48 Smallmouth bass 1 5 6 5 2 2 13 9 Largemouth bass 1 2 2 2 7 White crappie 2 1 Black crappie Chesapeake logperch 2 TotalCPUE 2,077 74 48 932 41 363 112 176 Total species 8 11 10 14 10 12 13 15 174

Final Report PBAPS Thermal Study Table 5-87. CPUE (number/O.Shr) and water temperature for fishes collected with a boat electrofisher at Station 190, July and August 2010-2013.

2010 2011 2012 2013 Ju~ August Ju~ August July Au~t Ju~ A~ust Collection water temperature ("C) 29.5 30 33.9 28.7 30.l 29.3 31.5 26.5 Gizlard shad 445 19 26 1,045 12 22 19 8 Common carp 2 3 Golden shiner 6 2 1 4 Comely shiner 14 5 9 20 25 39 11 7 Spottail shiner 1 3 3 Spotfin shiner 7 7 15 31 1 2 26 6 Bluntnose minnow 2 7 1 19 2 Channel catfish 6 17 13 18 12 22 36 59 Flathead catfJSh 1 Rock bass 1 Green sunf1Sh 6 28 4 77 31 44 67 106 Bluegill 14 39 1 46 26 286 24 58 Smallmouth bass 5 4 6 3 11 2 66 13 Largemouth bass 3 3 Greenside darter Tessellated darter Yellow perch 1 Chesapeake logperch 1 1 1 10 9 TotalCPUE 504 124 75 1,257 123 423 283 273 Total species 9 IO 8 12 10 11 12 12 175

Final Report PBAPS Thermal Study Table 5-88. CPUE (number/0.5hr) and water temperature for fishes collected with a boat electrofisher at Station 217, July and August 2010-2013.

2011 2012 2013 July August July August July August Collection water temperature ( C) 0 33.9 29.8 30.5 28.4 31.5 26.l Gi.12.ard shad 1,051 2,050 259 18 15 22 Common carp 3 1 3 5 Golden shiner 13 7 13 8 Comely shiner 2 14 61 47 4 Spottail shiner 14 2 2 Spotfin shiner 12 26 7 2 Bluntnose minnow 2 3 9 1 5 Creek chub White sucker 1 1 Northern hogsucker 3 3 Shorthead redhorse 1 4 11 15 9 Channel catfish 6 31 23 20 9 32 Flathead catfish 2 1 Rock bass 4 3 8 3 Redbreast sunfish Green sunfish 11 305 13 562 13 25 Bluegill 16 55 47 2,767 61 108 Smallmouth bass 6 3 10 3 55 21 Largemouth bass 4 1 2 15 White crappie 2 Greenside darter 2 Tessellated darter 2 Chesapeake logperch 4 9 10 12 9 28 Shield darter 2 Walleye 1 TotalCPUE 1,123 2,520 462 3,474 183 288 Total species 13 11 14 10 16 18 176

Final Report PBAPS Thermal Study Table 5-89. CPUE (number/collection) and water temperature for fishes collected with a seine at Station 202, July and August 2010-2013.

2010 2011 2012 2013 Ju~ August July August July August Ju~ August Collection water temperature ( C) 0 28.5 27.0 28.4 26.6 28.7 28.8 28.7 25.3 Gimlrd shad 1 Comely shiner 2 3 Common shiner 4 Spottail shiner 6 8 4 11 6 18 45 Spotfin shiner 13 17 11 12 14 8 6 8 Bluntnose minnow 6 9 12 19 15 4 Fallfish 2 Quillback 2 51 Northern hogsucker Shorthead redhorse 2 Channel catfish 1 Banded killifish Rock bass l Bluegill 1 31 30 9 Smallmouth bass 1 2 1 2 2 Tessellated darter 6 11 15 Chesapeake logperch 1 Tota!CPUE 31 75 81 70 17 62 45 63 Total species 8 7 6 7 4 8 8 7 177

Final Report PBAPS Thermal Study Table 5-90. CPUE (number/collection) and water temperature for fishes collected with a seine at Station 203, July and August 2010-2013.

2010 2011 2012 2013 Ju~ August Ju~ A~ust July Au~ust July A~ust Collection water tem~rature ("C) 28 26.5 27.6 25.3 28 28.9 28 25.4 Gizzard shad 1 2 3 3 River chub 2 Comely shiner 1 5 Spottail shiner 7 11 3 35 8 41 20 Swallowtail shiner 1 2 Spotfin shiner 4 9 3 4 1 3 14 5 Bluntnose minnow 1 16 86 1 35 FallflSh 1 5 Quillback Northern hogsucker 2 Shorthead redhorse 1 Channel catfish 2 Banded killifJSh Green sunfJSh Bluegill 4 23 Smallmouth bass 1 2 Largemouth bass 8 TotalCPUE 16 33 29 131 37 31 93 30 Total species 7 6 5 9 2 IO 5 3 178