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4-3 TOC-1 SS.CýýCooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 LIST OF FIGURES Figure 1 Figure 2 Figure 3 Figure 4 Figure 5 Site Location Map Site Layout Map Groundwater Flow Map Groundwater Analytical Results Summary March 4, 2009 Geologic Cross Section BLES Monitoring Well Construction Summary Water Level Measurements Analytical Results -Water Samples LIST OF TA]Table 1 Table 2 Table 3 LIST OF APPENDICES Appendix A Appendix B Appendix C Appendix D Boring Logs NCDENR Well Construction Records Field Notes Calculations TOC-2 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 1 INTRODUCTION | 4-3 TOC-1 SS.CýýCooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 LIST OF FIGURES Figure 1 Figure 2 Figure 3 Figure 4 Figure 5 Site Location Map Site Layout Map Groundwater Flow Map Groundwater Analytical Results Summary March 4, 2009 Geologic Cross Section BLES Monitoring Well Construction Summary Water Level Measurements Analytical Results -Water Samples LIST OF TA]Table 1 Table 2 Table 3 LIST OF APPENDICES Appendix A Appendix B Appendix C Appendix D Boring Logs NCDENR Well Construction Records Field Notes Calculations TOC-2 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 1 INTRODUCTION 1.1 Purpose of Report Silar Services Incorporated (SSi) has prepared this Cooling Tower Blowdown Line (CTBL) Assessment Report to document the results of investigation activities performed along a section of the CTBL at the Shearon Harris Nuclear Power Plant (SL{NPP), located in New Hill, North Carolina. | ||
of Report Silar Services Incorporated (SSi) has prepared this Cooling Tower Blowdown Line (CTBL) Assessment Report to document the results of investigation activities performed along a section of the CTBL at the Shearon Harris Nuclear Power Plant (SL{NPP), located in New Hill, North Carolina. | |||
The purpose of the assessment was to identify the potential presence and extent of radiological materials in groundwater within the assessment area of the line with respect to the integrity of the line.The initial assessment activities were conducted at the Site from January 21, 2009 through March 4, 2009. This Assessment Report, issued on April 1, 2009, provides a presentation of the activities completed and the findings of the assessment. | The purpose of the assessment was to identify the potential presence and extent of radiological materials in groundwater within the assessment area of the line with respect to the integrity of the line.The initial assessment activities were conducted at the Site from January 21, 2009 through March 4, 2009. This Assessment Report, issued on April 1, 2009, provides a presentation of the activities completed and the findings of the assessment. | ||
1.2 Project Background This section includes information on the location, description and history of the Site.1.2.1 Project Location The Shearon Harris Nuclear Power Plant is located approximately 1.6-miles east of the Town of New Hill, North Carolina, and is situated on approximately 10,700 acres site.The Site location is depicted on Figure 1.The Cooling Tower Blowdown Line, which is buried several feet below the ground surface, runs for approximately 2 miles from the cooling tower south to the edge of Harris Lake. The line assessment area is located between Air Release System Manhole#1 (ARS#l) which is located adjacent to the composite sampler shed (approximately 0.5 miles from the cooling tower) to ARS#2, located approximately 1,110 feet south of ARS#1. The assessment area is also depicted on Figure 1.1-1 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 1.2.2 Project Background On December 15, 2008, Progress Energy personnel discovered the presence of water in ARS#2. The manhole was investigated by purging the water from the manhole and evaluating conditions. | |||
Background This section includes information on the location, description and history of the Site.1.2.1 Project Location The Shearon Harris Nuclear Power Plant is located approximately 1.6-miles east of the Town of New Hill, North Carolina, and is situated on approximately 10,700 acres site.The Site location is depicted on Figure 1.The Cooling Tower Blowdown Line, which is buried several feet below the ground surface, runs for approximately 2 miles from the cooling tower south to the edge of Harris Lake. The line assessment area is located between Air Release System Manhole#1 (ARS#l) which is located adjacent to the composite sampler shed (approximately | |||
from the cooling tower) to ARS#2, located approximately 1,110 feet south of ARS#1. The assessment area is also depicted on Figure 1.1-1 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 1.2.2 Project Background On December 15, 2008, Progress Energy personnel discovered the presence of water in ARS#2. The manhole was investigated by purging the water from the manhole and evaluating conditions. | |||
It was observed that subsequent to purging the manhole dry, water was continuing to enter the bottom of the manhole through a 2-inch pipe designed to drain the manhole. A water sample was collected and analyzed for tritium. Tritium was detected at an approximate concentration of 800 pCi/l. Based on these observations, Progress Energy determined that additional evaluation was warranted. | It was observed that subsequent to purging the manhole dry, water was continuing to enter the bottom of the manhole through a 2-inch pipe designed to drain the manhole. A water sample was collected and analyzed for tritium. Tritium was detected at an approximate concentration of 800 pCi/l. Based on these observations, Progress Energy determined that additional evaluation was warranted. | ||
1.3 Scope and Objectives The overall objectives of the Cooling Tower Blowdown Line Assessment are as follows: " Characterize the hydrogeology and geology in the area* Provide groundwater sampling and elevation measuring points* Evaluate groundwater flow and groundwater quality* Assess potential sources of tritium concentration in water.The scope of the assessment included the collection of data as close as reasonably possible to the Cooling Tower Blowdown Line while not compromising the integrity of the line.1.4 Report Organization The organization and content of the remainder of this report are described below.Section 2.0 -Investigation Activities and Findings A summary of the activities completed during planning and implementation of the assessment is provided. | |||
and Objectives The overall objectives of the Cooling Tower Blowdown Line Assessment are as follows: " Characterize the hydrogeology and geology in the area* Provide groundwater sampling and elevation measuring points* Evaluate groundwater flow and groundwater quality* Assess potential sources of tritium concentration in water.The scope of the assessment included the collection of data as close as reasonably possible to the Cooling Tower Blowdown Line while not compromising the integrity of the line.1.4 Report Organization The organization and content of the remainder of this report are described below.Section 2.0 -Investigation Activities and Findings A summary of the activities completed during planning and implementation of the assessment is provided. | |||
The methods, locations, and results of the sampling and analysis program are presented in detail for soil and groundwater. | The methods, locations, and results of the sampling and analysis program are presented in detail for soil and groundwater. | ||
1-2 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 Section 3.0 -Physical Characteristics of the Study Area A description of the study area including surface features, geology and soils, surface water hydrology, and groundwater hydrology is provided in Section 3.Section 4.0 -Summary and Conclusions A summary of the relevant environmental conditions to satisfy the objectives of the investigation is provided in Section 4.2 ASSESSMENT ACTIVITIES AND FINDINGS The planning of the assessment activities included a number of conference calls and meetings with appropriate plant personnel. | 1-2 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 Section 3.0 -Physical Characteristics of the Study Area A description of the study area including surface features, geology and soils, surface water hydrology, and groundwater hydrology is provided in Section 3.Section 4.0 -Summary and Conclusions A summary of the relevant environmental conditions to satisfy the objectives of the investigation is provided in Section 4.2 ASSESSMENT ACTIVITIES AND FINDINGS The planning of the assessment activities included a number of conference calls and meetings with appropriate plant personnel. | ||
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* The horizontal migration of tritium in groundwater from the blowdown line appears to be limited as no tritium was detected in samples from BDL-MW8 and BDL-MW9.* The vertical migration of tritium in groundwater from the blowdown line appears to be limited as no tritium was detected in the sample from BDL-MW7.2-8 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 The highest concentration of zinc was detected in the sample from ARS#2 at a concentration of 187 ug/l, lower concentrations of zinc were detected in samples from BDL-MW8 (96 ug/h), BDL-MW5 (18 ug/1) and BDL-MW1 (8 ug/1).Based on the occurrence and distribution of tritium in the water samples, it appears that the source of tritium is a leak(s) along the Cooling Tower Blowdown Line. Analysis of the hydrogeology and groundwater conditions within the area is presented and discussed in Section 3, and further discussion regarding the possible sources of tritium is presented in Section 4. Conclusions and potential additional activities that may be performed to further evaluate the blowdown line are also presented in Section 4.2.3 Surveying and Mapping A site survey was performed and certified by a North Carolina Registered Land Surveyor (Smith and Smith). Initial surveying activities were performed on January 22, 2009 during which time the centerline of the Cooling Tower Blowdown Line was located and demarcated. | * The horizontal migration of tritium in groundwater from the blowdown line appears to be limited as no tritium was detected in samples from BDL-MW8 and BDL-MW9.* The vertical migration of tritium in groundwater from the blowdown line appears to be limited as no tritium was detected in the sample from BDL-MW7.2-8 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 The highest concentration of zinc was detected in the sample from ARS#2 at a concentration of 187 ug/l, lower concentrations of zinc were detected in samples from BDL-MW8 (96 ug/h), BDL-MW5 (18 ug/1) and BDL-MW1 (8 ug/1).Based on the occurrence and distribution of tritium in the water samples, it appears that the source of tritium is a leak(s) along the Cooling Tower Blowdown Line. Analysis of the hydrogeology and groundwater conditions within the area is presented and discussed in Section 3, and further discussion regarding the possible sources of tritium is presented in Section 4. Conclusions and potential additional activities that may be performed to further evaluate the blowdown line are also presented in Section 4.2.3 Surveying and Mapping A site survey was performed and certified by a North Carolina Registered Land Surveyor (Smith and Smith). Initial surveying activities were performed on January 22, 2009 during which time the centerline of the Cooling Tower Blowdown Line was located and demarcated. | ||
On February 20, 2009 all monitoring wells, manhole ARS#1, and manhole ARS#2 were surveyed.A survey map was produced that includes scale, benchmarks, North arrow, and the locations of monitoring wells. The survey map provided the information required to produce a site basemap for this Assessment Report.2-9 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant tý April 2009 3 PHYSICAL CHARACTERISTICS OF THE STUDY AREA This section presents the physical characteristics of the Site including surface features, geology, surface water hydrology, and groundwater hydrology. | On February 20, 2009 all monitoring wells, manhole ARS#1, and manhole ARS#2 were surveyed.A survey map was produced that includes scale, benchmarks, North arrow, and the locations of monitoring wells. The survey map provided the information required to produce a site basemap for this Assessment Report.2-9 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant tý April 2009 3 PHYSICAL CHARACTERISTICS OF THE STUDY AREA This section presents the physical characteristics of the Site including surface features, geology, surface water hydrology, and groundwater hydrology. | ||
3.1 Surface Features The SHNPP is located approximately 1.6 miles east of the town of New Hill, North Carolina. | |||
Access to the SHNPP is from Shearon Harris Road. The owner controlled area encompasses approximately 10,700 acres. The area of the Cooling Tower Blowdown Line, which is the focus of this assessment, includes approximately 15 acres.As discussed in Section 1, the Cooling Tower Blowdown Line runs underground for approximately 2 miles from the Cooling Tower south to the edge of Harris Lake. The assessment area is on a peninsula which is surrounded by Harris Lake to the south, east, and west and bounded to the north by SHNPP. Specifically, the blowdown line assessment area is located between ARS#1, located adjacent to the composite sampler shed (approximately 0.5 miles from the cooling tower), to ARS#2 which is located approximately 1,110 feet south of ARS# 1. The most significant surface feature in the assessment area is the topographic low area/wetlands, situated along the blowdown line approximately midway between ARS#1 and ARS#2. There is an approximately 30-foot elevation change between ARS#1 and the topographic low to the south. In addition, a portion of Harris Lake is located east of manhole ARS#2.The Site location is shown on Figure 1, and the Site Layout is depicted on Figure 2.3.2 Geology Regional and site-specific geology have been extensively evaluated by others during the safety analyses for Unit 1 and more recently for proposed Units 2 and 3. These reports indicate that the plant is underlain by the Upper Triassic Age Newark Supergroup. | |||
Features The SHNPP is located approximately | |||
east of the town of New Hill, North Carolina. | |||
Access to the SHNPP is from Shearon Harris Road. The owner controlled area encompasses approximately 10,700 acres. The area of the Cooling Tower Blowdown Line, which is the focus of this assessment, includes approximately 15 acres.As discussed in Section 1, the Cooling Tower Blowdown Line runs underground for approximately 2 miles from the Cooling Tower south to the edge of Harris Lake. The assessment area is on a peninsula which is surrounded by Harris Lake to the south, east, and west and bounded to the north by SHNPP. Specifically, the blowdown line assessment area is located between ARS#1, located adjacent to the composite sampler shed (approximately | |||
from the cooling tower), to ARS#2 which is located approximately 1,110 feet south of ARS# 1. The most significant surface feature in the assessment area is the topographic low area/wetlands, situated along the blowdown line approximately midway between ARS#1 and ARS#2. There is an approximately 30-foot elevation change between ARS#1 and the topographic low to the south. In addition, a portion of Harris Lake is located east of manhole ARS#2.The Site location is shown on Figure 1, and the Site Layout is depicted on Figure 2.3.2 Geology Regional and site-specific geology have been extensively evaluated by others during the safety analyses for Unit 1 and more recently for proposed Units 2 and 3. These reports indicate that the plant is underlain by the Upper Triassic Age Newark Supergroup. | |||
The 3-1 Cooling Tower Blowdown Line Assessment Report 8 8 .Shearon Harris Nuclear Power Plant April 2009 group is characterized by siltstone and sandstone with subordinate amounts of claystone and conglomerated and igneous diabase intrusions. | The 3-1 Cooling Tower Blowdown Line Assessment Report 8 8 .Shearon Harris Nuclear Power Plant April 2009 group is characterized by siltstone and sandstone with subordinate amounts of claystone and conglomerated and igneous diabase intrusions. | ||
Additional information on regional and local geology can be found in the Final Safety Analysis Report (FSAR).Site-specific geology observed in the area of the blowdown line is consistent with the regional geology. Soil borings encountered a thin layer of unconsolidated material (overburden), underlain by a reddish-brown weathered siltstone bedrock (regolith) underlain by reddish-brown siltstone. | Additional information on regional and local geology can be found in the Final Safety Analysis Report (FSAR).Site-specific geology observed in the area of the blowdown line is consistent with the regional geology. Soil borings encountered a thin layer of unconsolidated material (overburden), underlain by a reddish-brown weathered siltstone bedrock (regolith) underlain by reddish-brown siltstone. | ||
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Therefore, eight (8) shallow (less than 30 feet bgs) and one (1) deep (approximately 60 feet bgs) wells were installed during the assessment. | Therefore, eight (8) shallow (less than 30 feet bgs) and one (1) deep (approximately 60 feet bgs) wells were installed during the assessment. | ||
One complete round of water level measurements was collected. | One complete round of water level measurements was collected. | ||
Those water level measurements and resulting elevations are shown on Figure 3. Groundwater elevations are also shown on the geologic cross-section included as Figure 5. As indicated, the groundwater elevations are highly variable 3-2 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 particularly in the area of ARS#2. General observations regarding the assessment area groundwater are as follows: " In the area of ARS#l, as characterized by BDL-MW1 through BDL-MW3, groundwater elevations indicate flow to the south toward the topographic low/wetland." In the area of ARS#2, water was detected in BDL-MW5 and BDL-MW6 several days after the wells were installed, however BDL-MW4 remains dry. This indicates that the water observed in BDL-MW5 and BDL-MW6 is not from a local/regional groundwater source.* The water elevation in ARS#2 is higher than that in BDL-MW5 and BDL-MW6 indicating that flow is from the immediate vicinity of ARS#2 to these monitoring wells and not from a local/regional groundwater source.* In the area of ARS#2, groundwater was detected in BDL-MW7 at a significantly lower elevation that the water levels detected in BDL-MW5 and BDL-MW6, indicating that the regional groundwater elevation may be significantly lower than the water level observed in BDL-MW5 and BDL-MW6.* The groundwater elevation at BDL-MW8 was measured to be at or above the ground surface indicating local artesian conditions at this location.* The groundwater elevation at BDL-MW9, which is located approximately 40 feet from the edge of Harris Lake, was measure at an elevation | Those water level measurements and resulting elevations are shown on Figure 3. Groundwater elevations are also shown on the geologic cross-section included as Figure 5. As indicated, the groundwater elevations are highly variable 3-2 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 particularly in the area of ARS#2. General observations regarding the assessment area groundwater are as follows: " In the area of ARS#l, as characterized by BDL-MW1 through BDL-MW3, groundwater elevations indicate flow to the south toward the topographic low/wetland." In the area of ARS#2, water was detected in BDL-MW5 and BDL-MW6 several days after the wells were installed, however BDL-MW4 remains dry. This indicates that the water observed in BDL-MW5 and BDL-MW6 is not from a local/regional groundwater source.* The water elevation in ARS#2 is higher than that in BDL-MW5 and BDL-MW6 indicating that flow is from the immediate vicinity of ARS#2 to these monitoring wells and not from a local/regional groundwater source.* In the area of ARS#2, groundwater was detected in BDL-MW7 at a significantly lower elevation that the water levels detected in BDL-MW5 and BDL-MW6, indicating that the regional groundwater elevation may be significantly lower than the water level observed in BDL-MW5 and BDL-MW6.* The groundwater elevation at BDL-MW8 was measured to be at or above the ground surface indicating local artesian conditions at this location.* The groundwater elevation at BDL-MW9, which is located approximately 40 feet from the edge of Harris Lake, was measure at an elevation | ||
(-210 feet MSL)approximately 10 feet below the surface water level indicating that surface water from Harris Lake may be discharging to groundwater in this area.3-3 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 4 | (-210 feet MSL)approximately 10 feet below the surface water level indicating that surface water from Harris Lake may be discharging to groundwater in this area.3-3 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 4 | ||
==SUMMARY== | ==SUMMARY== | ||
AND CONCLUSIONS Silar Services Incorporated (SSi) has prepared this Cooling Tower Blowdown Line Assessment Report to document the results of investigation activities performed along a section of the line at the Shearon Harris Nuclear Power Plant, located in New Hill, North Carolina. | AND CONCLUSIONS Silar Services Incorporated (SSi) has prepared this Cooling Tower Blowdown Line Assessment Report to document the results of investigation activities performed along a section of the line at the Shearon Harris Nuclear Power Plant, located in New Hill, North Carolina. | ||
The purpose of the assessment was to identify the potential presence and extent of radiological materials in groundwater within the area of the line with respect to the integrity of the line.The Cooling Tower Blowdown Line runs underground for approximately 2 miles from the cooling tower south to the edge of Harris Lake. The line assessment area is located between Air Release System Manhole #1 (ARS#1), which is located adjacent to the composite sampler shed (approximately | The purpose of the assessment was to identify the potential presence and extent of radiological materials in groundwater within the area of the line with respect to the integrity of the line.The Cooling Tower Blowdown Line runs underground for approximately 2 miles from the cooling tower south to the edge of Harris Lake. The line assessment area is located between Air Release System Manhole #1 (ARS#1), which is located adjacent to the composite sampler shed (approximately 0.5 miles from the cooling tower), to ARS#2, located approximately 1,110 feet south of ARS#1. The overall objectives of the Cooling Tower Blowdown Line assessment are as follows:* Characterize the hydrogeology and geology in the area* Provide groundwater sampling and elevation measuring points* Evaluate groundwater flow and groundwater quality" Assess potential sources of tritium concentration in water.<The assessment field activities were completed intwo phases. The first phase included the foll6owing activities: | ||
from the cooling tower), to ARS#2, located approximately 1,110 feet south of ARS#1. The overall objectives of the Cooling Tower Blowdown Line assessment are as follows:* Characterize the hydrogeology and geology in the area* Provide groundwater sampling and elevation measuring points* Evaluate groundwater flow and groundwater quality" Assess potential sources of tritium concentration in water.<The assessment field activities were completed intwo phases. The first phase included the foll6owing activities: | |||
* Installation of six (6) groundwater monitoring wells BDL-MWl through BDL-MW6 atMpoints along the blowdown line and ARS#2.; <Collection of preliminary groundwater, samples from BDL-MWl; BD-MW2, and BDL-MW-3.," Water level measurements and preliminay groundwater samples from ~BDL-MW5 and BDL-MW6.4-1 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 The scon~d h&&iasfhe aseset included:-Installation of three (3) groundwater monitormg wellsr BDL-MW7. through BDL-MW9at S#2 and toward Harris Lake." Measuirinig water, level elevations." Collecting a complete round of water samples from the mon~itoring wells~ and ARS1#2.1 4.1 Summary of Groundwater Conditions Groundwater samples were collected from the monitoring wells (8 samples) and manhole (1 sample) and analyzed for tritium. Samples from BDL-MW1, BDL-MW5, BDL-MW8, and ARS#2 were also analyzed for zinc, since zinc is added to the cooling water and can be used as a marker analyte. Tritium was detected in five (5) of the eight (8) monitoring wells sampled and in the ARS#2 sample at concentrations up to 2,120 pCi/L. (detected at ARS#2).The highest .concentration of tritium detected in the samples was detected in the immediate area of ARS#2 (ARS#2, BDL-MW5, and BDL-MW6). | * Installation of six (6) groundwater monitoring wells BDL-MWl through BDL-MW6 atMpoints along the blowdown line and ARS#2.; <Collection of preliminary groundwater, samples from BDL-MWl; BD-MW2, and BDL-MW-3.," Water level measurements and preliminay groundwater samples from ~BDL-MW5 and BDL-MW6.4-1 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 The scon~d h&&iasfhe aseset included:-Installation of three (3) groundwater monitormg wellsr BDL-MW7. through BDL-MW9at S#2 and toward Harris Lake." Measuirinig water, level elevations." Collecting a complete round of water samples from the mon~itoring wells~ and ARS1#2.1 4.1 Summary of Groundwater Conditions Groundwater samples were collected from the monitoring wells (8 samples) and manhole (1 sample) and analyzed for tritium. Samples from BDL-MW1, BDL-MW5, BDL-MW8, and ARS#2 were also analyzed for zinc, since zinc is added to the cooling water and can be used as a marker analyte. Tritium was detected in five (5) of the eight (8) monitoring wells sampled and in the ARS#2 sample at concentrations up to 2,120 pCi/L. (detected at ARS#2).The highest .concentration of tritium detected in the samples was detected in the immediate area of ARS#2 (ARS#2, BDL-MW5, and BDL-MW6). | ||
The next highest concentration of tritium was detected at BDL-MW3, near the wetland in the area of groundwater discharge. | The next highest concentration of tritium was detected at BDL-MW3, near the wetland in the area of groundwater discharge. | ||
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>This evaluation assumes tritiated groun dwater is introdtuiced from ARS#2' to~ the environment at a.concentration of approximately 1,260 pji/L (tritium concentration detected in water*samled from located downgradient of ARS#2). Once introduced into they environment tritiatedjgroundwater flows east northeast toward e the.. owner-.controlled area boundary at a rate of ThAppendixD). | >This evaluation assumes tritiated groun dwater is introdtuiced from ARS#2' to~ the environment at a.concentration of approximately 1,260 pji/L (tritium concentration detected in water*samled from located downgradient of ARS#2). Once introduced into they environment tritiatedjgroundwater flows east northeast toward e the.. owner-.controlled area boundary at a rate of ThAppendixD). | ||
The owner-controlled area: boundary in the !general direction of groundwater flow is approximately 1.79 milesj or 9,45 1 feet from the ARS#2 ~area.. Based on these estimates it would take groundwater from the ARS#2 area a~pproximately 49 ~years to ~reachi the 4-2 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 ownter con ITO Iboundary. | The owner-controlled area: boundary in the !general direction of groundwater flow is approximately 1.79 milesj or 9,45 1 feet from the ARS#2 ~area.. Based on these estimates it would take groundwater from the ARS#2 area a~pproximately 49 ~years to ~reachi the 4-2 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 ownter con ITO Iboundary. | ||
Based on Ihec ha If-life of tntiurn (12.3:3 yearstfow rate (193'~ft/year), distancee | Based on Ihec ha If-life of tntiurn (12.3:3 yearstfow rate (193'~ft/year), distancee | ||
(;9,451 eet) inital rtim m:concentration | (;9,451 eet) inital rtim m:concentration | ||
ýmn te environment! | ýmn te environment! | ||
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BDL-MW-1 STATE WELL PERMIT#(if applicable)_ | BDL-MW-1 STATE WELL PERMIT#(if applicable)_ | ||
DWQ or OTHER PERMIT #*lf applicable) | DWQ or OTHER PERMIT #*lf applicable) | ||
WELL USE (Check Applicable Box) Monitoring 9] Municipal/Public 0 Industrial/Commercial | WELL USE (Check Applicable Box) Monitoring 9] Municipal/Public 0 Industrial/Commercial | ||
[3 Agricultural | [3 Agricultural | ||
[I Recovery D Injection 0 IrrigationC3 Other 0 (list use)DATE DRILLED 01/22/09 TIME COMPLETED | [I Recovery D Injection 0 IrrigationC3 Other 0 (list use)DATE DRILLED 01/22/09 TIME COMPLETED | ||
-AMO PMQ 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbera, Community, Subdivision, Lot No., Parcel, Zip Code)TOPOGRAPHIC | -AMO PMQ 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbera, Community, Subdivision, Lot No., Parcel, Zip Code)TOPOGRAPHIC | ||
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BDL-MW-2 STATE WELL PERMIT#(if applicable) | BDL-MW-2 STATE WELL PERMIT#(if applicable) | ||
DWO or OTHER PERMIT #(if applicable)_ | DWO or OTHER PERMIT #(if applicable)_ | ||
WELL USE (Check Applicable Box) Monitoring | WELL USE (Check Applicable Box) Monitoring | ||
: 8) Municipal/Public | : 8) Municipal/Public | ||
[I Industrial/Commerciai 0 Agricultural 0 Recovery 0] Injection | [I Industrial/Commerciai 0 Agricultural 0 Recovery 0] Injection | ||
[0 Irrigationo Other 0 (list use)__ _DATE DRILLED 0117.2./09 TIME COMPLETED AM n PM r 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbers, Community, Subdfivsion, Lot No., Parcel, Zip Code)TOPOGRAPHIC | [0 Irrigationo Other 0 (list use)__ _DATE DRILLED 0117.2./09 TIME COMPLETED AM n PM r 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbers, Community, Subdfivsion, Lot No., Parcel, Zip Code)TOPOGRAPHIC | ||
/ LAND SETTING: OSIope OValley 0Flat []Ridge 0 Other (check appropriate box)LATITUDE _ May be in degrees, minutes, seconds or LONGITUDE in a decimal format Latitude/longitude source: oGPS oTopographic map'(location of wel must be shown on e USGS topo map and attached to this form if not using GPS)4. FACIUTY. Is the name of the business where the well Is located.FACILITY ID #(if applicable) | / LAND SETTING: OSIope OValley 0Flat []Ridge 0 Other (check appropriate box)LATITUDE _ May be in degrees, minutes, seconds or LONGITUDE in a decimal format Latitude/longitude source: oGPS oTopographic map'(location of wel must be shown on e USGS topo map and attached to this form if not using GPS)4. FACIUTY. Is the name of the business where the well Is located.FACILITY ID #(if applicable) | ||
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BDL-MW-5 STATE WELL PERMIT#(if applicable) | BDL-MW-5 STATE WELL PERMIT#(if applicable) | ||
_ _ _DWQ or OTHER PERMIT #(if applicable)_ | _ _ _DWQ or OTHER PERMIT #(if applicable)_ | ||
WELL USE (Check Applicable Box) Monitoring | WELL USE (Check Applicable Box) Monitoring | ||
[J MunicipaV/Public | [J MunicipaV/Public | ||
[I Industrial/Commercial 0 Agricultural | [I Industrial/Commercial 0 Agricultural | ||
[I Recovery[) | [I Recovery[) | ||
Irjection D Irrigationo Other C (list use)DATE DRILLED 01127/09 TIME COMPLETED AM 0 PM 0 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbers, Community, Subdhision, Lot No., Parcel, Zip Code)TOPOGRAPHIC | Irjection D Irrigationo Other C (list use)DATE DRILLED 01127/09 TIME COMPLETED AM 0 PM 0 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbers, Community, Subdhision, Lot No., Parcel, Zip Code)TOPOGRAPHIC |
Revision as of 23:48, 30 April 2019
ML102030160 | |
Person / Time | |
---|---|
Site: | Harris |
Issue date: | 04/30/2009 |
From: | Silar Services |
To: | Office of Information Services, Progress Energy Carolinas |
References | |
FOIA/PA-2010-0209 | |
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COOLING TOWER BLOWDOWN LINE ASSESSMENT REPORT SHEARON HARRIS NUCLEAR POWER PLANT NEW HILL, NORTH CAROLINA PREPARED FOR: PROGRESS ENERGY CAROLINAS PREPARED BY: Ss§4 SILAR SERVICES, INC.'.983 BUTLER PIKE BLUE BELL, PA 19422.April 2009 e COOLING TOWER BLOWDOWN LINE ASSESSMENT REPORT SHEARON HARRIS NUCLEAR POWER PLANT NEW HILL, NORTH CAROLINA PREPARED FOR: PROGRESS ENERGY CAROLINAS PREPARED BY: ss.SILAR SERVICES, INC.983 BUTLER PIKE BLUE BELL, PA 19422 April 2009 Cooling Tower Blowdown Line Assessment Report Sss Shearon Harris Nuclear Power Plant April 2009 TABLE OF CONTENTS INTRODUCTION
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1-1 1.1 Purpose of R eport .......................................................................
1-1 1.2 Project Background
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1-1 1.2.1 Project L ocation ...........................................................................
1-1 1.2.2 Project B ackground
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1-2 1.3 Scope and Objectives
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1-2 1.4 Report Organization
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1-2 2 ASSESSMENT ACTIVITIES AND FINDINGS ...........................
2-3 2.1 Assessment Activities
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2-4 2.1.1 Soil Borings/Groundwater Monitoring Well Installation
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2-4 2.1.2 Groundwater Elevation Measurements
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2-6 2.1.3 G roundw ater Sam pling ...............................................................
2-6 2.2 Assessment Findings -Water Results ........................................
2-8 2.3 Surveying and Mapping ..............................................................
2-9 3 PHYSICAL CHARACTERISTICS OF THE STUDY AREA ..... 3-1 3.1 Surface Features ..........................................................................
3-1 3 .2 G eology .......................................................................................
3-1 3.3 Groundwater Hydrology
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3-2 4
SUMMARY
AND CONCLUSIONS
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4-1 4.1 Summary of Groundwater Conditions
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4-2 4.2 C onclusions
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4-3 TOC-1 SS.CýýCooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 LIST OF FIGURES Figure 1 Figure 2 Figure 3 Figure 4 Figure 5 Site Location Map Site Layout Map Groundwater Flow Map Groundwater Analytical Results Summary March 4, 2009 Geologic Cross Section BLES Monitoring Well Construction Summary Water Level Measurements Analytical Results -Water Samples LIST OF TA]Table 1 Table 2 Table 3 LIST OF APPENDICES Appendix A Appendix B Appendix C Appendix D Boring Logs NCDENR Well Construction Records Field Notes Calculations TOC-2 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 1 INTRODUCTION 1.1 Purpose of Report Silar Services Incorporated (SSi) has prepared this Cooling Tower Blowdown Line (CTBL) Assessment Report to document the results of investigation activities performed along a section of the CTBL at the Shearon Harris Nuclear Power Plant (SL{NPP), located in New Hill, North Carolina.
The purpose of the assessment was to identify the potential presence and extent of radiological materials in groundwater within the assessment area of the line with respect to the integrity of the line.The initial assessment activities were conducted at the Site from January 21, 2009 through March 4, 2009. This Assessment Report, issued on April 1, 2009, provides a presentation of the activities completed and the findings of the assessment.
1.2 Project Background This section includes information on the location, description and history of the Site.1.2.1 Project Location The Shearon Harris Nuclear Power Plant is located approximately 1.6-miles east of the Town of New Hill, North Carolina, and is situated on approximately 10,700 acres site.The Site location is depicted on Figure 1.The Cooling Tower Blowdown Line, which is buried several feet below the ground surface, runs for approximately 2 miles from the cooling tower south to the edge of Harris Lake. The line assessment area is located between Air Release System Manhole#1 (ARS#l) which is located adjacent to the composite sampler shed (approximately 0.5 miles from the cooling tower) to ARS#2, located approximately 1,110 feet south of ARS#1. The assessment area is also depicted on Figure 1.1-1 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 1.2.2 Project Background On December 15, 2008, Progress Energy personnel discovered the presence of water in ARS#2. The manhole was investigated by purging the water from the manhole and evaluating conditions.
It was observed that subsequent to purging the manhole dry, water was continuing to enter the bottom of the manhole through a 2-inch pipe designed to drain the manhole. A water sample was collected and analyzed for tritium. Tritium was detected at an approximate concentration of 800 pCi/l. Based on these observations, Progress Energy determined that additional evaluation was warranted.
1.3 Scope and Objectives The overall objectives of the Cooling Tower Blowdown Line Assessment are as follows: " Characterize the hydrogeology and geology in the area* Provide groundwater sampling and elevation measuring points* Evaluate groundwater flow and groundwater quality* Assess potential sources of tritium concentration in water.The scope of the assessment included the collection of data as close as reasonably possible to the Cooling Tower Blowdown Line while not compromising the integrity of the line.1.4 Report Organization The organization and content of the remainder of this report are described below.Section 2.0 -Investigation Activities and Findings A summary of the activities completed during planning and implementation of the assessment is provided.
The methods, locations, and results of the sampling and analysis program are presented in detail for soil and groundwater.
1-2 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 Section 3.0 -Physical Characteristics of the Study Area A description of the study area including surface features, geology and soils, surface water hydrology, and groundwater hydrology is provided in Section 3.Section 4.0 -Summary and Conclusions A summary of the relevant environmental conditions to satisfy the objectives of the investigation is provided in Section 4.2 ASSESSMENT ACTIVITIES AND FINDINGS The planning of the assessment activities included a number of conference calls and meetings with appropriate plant personnel.
A scope of work to complete the assessment objectives was prepared by SSi and submitted to Progress Energy on January 6, 2009. The initial scope of work called for the installation of up to 20 shallow (approximately 25 feet below ground surface or bgs) soil borings/monitoring wells to complete the study objectives.
The assessment field activities were completed in two phases. The first phase was completed from January 21 to February 6, 2009, and included the following activities: " Installation of six (6) groundwater monitoring wells BDL-MW1 through BDL-MW6 at points along the blowdown line and near ARS#2," Collection of preliminary groundwater samples from BDL-MW1, BDL-MW2, and BDL-MW-3 on January 23, 2009, and* Water level measurements and preliminary groundwater samples from BDL-MW5 and BDL-MW6 on February 6, 2009.Based on these initial activities and findings, the original scope of work was revised to reduce the number of wells due to the general absence of shallow groundwater.
The second phase of the assessment was completed from February 17 to March 4, 2009, and included: 2-3 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009" Installation of three (3) groundwater monitoring wells BDL-MW7 through BDL-MW9 at ARS#2 and downgradient of ARS#2 toward Harris Lake,* Measuring water level elevations on March 3, 2009, and* Collecting a complete round of water samples from the monitoring wells and ARS#2 on March 4, 2009.These activities are described in detail below. The locations of the groundwater monitoring wells installed in the area are depicted on Figure 2.The activities and findings are summarized in the following subsections.
The analytical results are presented and, where concentrations of radiological materials were observed, the results are also presented on figures. Throughout this section, groundwater data are discussed with respect to the USEPA drinking water standard of 20,000 pCi/L (picocuries per liter).2.1 Assessment Activities To accomplish the objectives of ote assessment, several investigatin actites complted including:
soil borings/monitoning well installation, groundwater elation me andgrounhwater, sampling.The assessment methods and, results, are, discussed in the following subsections.
Objective 1.3a Installation of .1 Soil] Boings/Groundwater' Monitoring Well Installation:
additional monitoring wells he primary objectives of the soil boring/monitoring well installation were to evaluate subsurface conditions and establish a network of monitoring wells in the Cooling Tower Blowdown Line assessment area to evaluate geology, hydrogeology and groundwater quality. To accomplish this objective, soil borings were advanced and monitoring wells were installed at the locations illustrated on Figure 2. Boreholes were logged from split spoon samples and cuttings.
The screened interval for each monitoring well was selected to intersect the depth intervals where groundwater was observed.
Where no groundwater was observed the bottom of the screened interval was 2-4 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 placed at the maximum penetration depth of the drilling technique and below observed water levels in the adjacent manholes.Hollow-stem auger (HSA) drilling methods were employed to complete the installation of groundwater monitoring wells BDL-MW1 through BDL-MW6. HSA and air rotary drilling methods were employed to complete the installation of groundwater monitoring wells BDL-MW7 through BDL-MW9. The drilling activities are described in the following sections.During the investigation, a total of nine (9) shallow groundwater monitoring wells were installed as shown on Figure 2. The general monitoring well installation procedures are summarized below." The depth for each of the wells was selected based on presence and depth of groundwater at each well location.
Where no groundwater was observed, the bottom of the well was set at the maximum drilling depth using the HSA techniques (BDL-MW 4 through BDL-MW6, only) and below the water level in ARS#2.* The wells were generally installed using 4'/4-inch inside diameter (ID)hollow stem augers and/or 4-inch air hammer.* At least ten feet of 2-inch-ID, Schedule 40 PVC, machine cut, well screen with 0.020-inch-slot size was set at the bottom of each well. A sufficient length of 2-inch ID, Schedule 40 PVC riser pipe was coupled to the screen to allow the PVC riser pipe to extend a minimum of two feet above the ground surface. Well screens were fitted with a nominal 2-inch solid (unslotted) bottom sediment trap.* The annular space around the well screens was backfilled with clean uniform sand (filter pack sieve #2). The filter pack was placed from the bottom of the well to a minimum of 2 feet above the top of the well screen. A minimum 2-foot-thick bentonite seal was placed above the sand and allowed to hydrate.* All wells were completed as stick-up wells, with lockable expansion plugs.2-5 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009" A concrete pad will be installed around the wells that are determined by Progress Energy and SSi to be completed as permanent wells.* Boring Logs were prepared for each monitoring well.A summary of the monitoring well construction details is provided in Table 1 and depicted in the Boring Logs included in Appendix A. NCDENR Well Construction Records are included in Appendix B.2.1.2 Groundwater Elevation Measurements Groundwater elevation measurements were collected from the monitoring wells and used to provide data to map the potentiometric surface of the aquifer and interpret the horizontal groundwater flow in the aquifer. One complete round of depth-to-water measurements was collected from the nine monitoring wells on March 3, 2009.Measurements were collected using a Solinst Level Indicator Probe capable of measuring depth to water within 0.01-foot accuracy.
Results of these measurements are summarized in Table 2, presented on Figure 3, and discussed in Section 3 of this report.2.1.3 Groundwater Sampling One round of groundwater samples was collected from the monitoring wells. All monitoring wells were sampled except BDL-MW4, which was dry. In addition, a water sample was collected directly from the drainpipe in manhole ARS#2. Water samples were analyzed for tritium at Progress Energy's Harris Energy and Environmental Center Radiochemistry Laboratory to the same lower limit of detection as the NC Division of Radiation Protection (NCDRP) laboratory.
In addition, select water samples were analyzed for total zinc.Prior to sampling, each monitoring well was purged in accordance with low-flow groundwater sampling procedures to assure collection of a representative groundwater sample. Groundwater sampling was completed using a peristaltic pump, dedicated 2-6 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant tý .April 2009 pump (flex) tubing, and dedicated down-hole polyethylene tubing at each monitoring well to eliminate the potential for cross-contamination between sampling points. Water quality measurements (pH, temperature, dissolved oxygen, conductivity, and oxidation/reduction potential) were collected during the purging activities and recorded in the field logbook (Appendix C). The procedure for monitoring well purging and sampling is generally as follows:* The security cap was removed, and the depth to water in the well was determined with a water level meter. The depth to water was recorded in the field logbook.* The dedicated down-hole tubing was lowered into the monitoring well, cut to the desired length, attached to the pre-cut flex tubing on the peristaltic pump, a new section of poly tubing was inserted on the effluent side of the pump. The sample line was connected from the pump to the in-line water quality instrument (YSI MP556 with flow through cell), the effluent line from the flow-through cell was inserted into a purge water container to capture purge water, the peristaltic pump was started, and purging of groundwater at the well was commenced.
- An optimum low-flow pumping rate was established at each well to minimize drawdown.
The groundwater quality parameters and depth to water were monitored and recorded at prescribed time intervals to determine when the water quality parameters had stabilized to within 10%.* Following the stabilization of the groundwater quality parameters, groundwater samples were collected from the wells and delivered to the radiological analytical laboratory.
- Purge water was collected and transported to the designated disposal point.ARS#2 was sampled in general accordance with the methodology specified above.2-7 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 2.2 Assessment Findings -Water Results Groundwater samples were collected from the monitoring wells on March 4, 2009. All water samples from the wells (8 samples) and manhole (I sample) were analyzed for tritium at the on-site radiological analytical laboratory.
Samples from BDL-MW1, BDL-MW5, BDL-MW8, and ARS#2 were also analyzed for zinc, since zinc is added to the cooling water and can be used as a marker analyte. Analytical results are summarized in Table 3. Figure 4 depicts the analytical results for tritium in the water samples. The results are summarized below.* Tritium was detected in five (5) of the eight (8) monitoring wells sampled and in the ARS#2 sample. The detection limit for the analyses was approximately 233 pCi/L.* Tritium in the nine (9) samples ranged from less than the detection limit (three wells) to 2,120 pCi/L at manhole ARS#2." The highest concentration of tritium detected in the samples was detected in the immediate area of ARS#2 (ARS#2, BDL-MW5, and BDL-MW6).
The second highest concentration of tritium was detected at BDL-MW3, near the wetland in the area of groundwater discharge.
These three wells are located in close proximity to the backfilled trench of the blowdown line which is likely acting as a preferential pathway of water transport.
- The horizontal migration of tritium in groundwater from the blowdown line appears to be limited as no tritium was detected in samples from BDL-MW8 and BDL-MW9.* The vertical migration of tritium in groundwater from the blowdown line appears to be limited as no tritium was detected in the sample from BDL-MW7.2-8 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 The highest concentration of zinc was detected in the sample from ARS#2 at a concentration of 187 ug/l, lower concentrations of zinc were detected in samples from BDL-MW8 (96 ug/h), BDL-MW5 (18 ug/1) and BDL-MW1 (8 ug/1).Based on the occurrence and distribution of tritium in the water samples, it appears that the source of tritium is a leak(s) along the Cooling Tower Blowdown Line. Analysis of the hydrogeology and groundwater conditions within the area is presented and discussed in Section 3, and further discussion regarding the possible sources of tritium is presented in Section 4. Conclusions and potential additional activities that may be performed to further evaluate the blowdown line are also presented in Section 4.2.3 Surveying and Mapping A site survey was performed and certified by a North Carolina Registered Land Surveyor (Smith and Smith). Initial surveying activities were performed on January 22, 2009 during which time the centerline of the Cooling Tower Blowdown Line was located and demarcated.
On February 20, 2009 all monitoring wells, manhole ARS#1, and manhole ARS#2 were surveyed.A survey map was produced that includes scale, benchmarks, North arrow, and the locations of monitoring wells. The survey map provided the information required to produce a site basemap for this Assessment Report.2-9 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant tý April 2009 3 PHYSICAL CHARACTERISTICS OF THE STUDY AREA This section presents the physical characteristics of the Site including surface features, geology, surface water hydrology, and groundwater hydrology.
3.1 Surface Features The SHNPP is located approximately 1.6 miles east of the town of New Hill, North Carolina.
Access to the SHNPP is from Shearon Harris Road. The owner controlled area encompasses approximately 10,700 acres. The area of the Cooling Tower Blowdown Line, which is the focus of this assessment, includes approximately 15 acres.As discussed in Section 1, the Cooling Tower Blowdown Line runs underground for approximately 2 miles from the Cooling Tower south to the edge of Harris Lake. The assessment area is on a peninsula which is surrounded by Harris Lake to the south, east, and west and bounded to the north by SHNPP. Specifically, the blowdown line assessment area is located between ARS#1, located adjacent to the composite sampler shed (approximately 0.5 miles from the cooling tower), to ARS#2 which is located approximately 1,110 feet south of ARS# 1. The most significant surface feature in the assessment area is the topographic low area/wetlands, situated along the blowdown line approximately midway between ARS#1 and ARS#2. There is an approximately 30-foot elevation change between ARS#1 and the topographic low to the south. In addition, a portion of Harris Lake is located east of manhole ARS#2.The Site location is shown on Figure 1, and the Site Layout is depicted on Figure 2.3.2 Geology Regional and site-specific geology have been extensively evaluated by others during the safety analyses for Unit 1 and more recently for proposed Units 2 and 3. These reports indicate that the plant is underlain by the Upper Triassic Age Newark Supergroup.
The 3-1 Cooling Tower Blowdown Line Assessment Report 8 8 .Shearon Harris Nuclear Power Plant April 2009 group is characterized by siltstone and sandstone with subordinate amounts of claystone and conglomerated and igneous diabase intrusions.
Additional information on regional and local geology can be found in the Final Safety Analysis Report (FSAR).Site-specific geology observed in the area of the blowdown line is consistent with the regional geology. Soil borings encountered a thin layer of unconsolidated material (overburden), underlain by a reddish-brown weathered siltstone bedrock (regolith) underlain by reddish-brown siltstone.
A site-specific interpretation of the geology in the area has been developed by using boring logs from the assessment activities and is presented as a cross-section on Figure 5.3.3 Groundwater Hydrology Regional and site-specific groundwater hydrology have been extensively evaluated by others during the safety analyses for Unit 1 and more recently for proposed Units 2 and 3. These reports indicate that the groundwater hydrology within the plant area is relatively complex as a result of the influence of the main and auxiliary reservoirs and the nature of the parent rock. The previous groundwater studies have focused on the plant area, located to the north of this assessment area. The nearest previously existing monitoring well is MWA-12, which is located approximately 1,000 feet northeast of ARS#l. Historic groundwater elevation at this location was approximately 235' MSL.Groundwater monitoring activities were performed during this assessment to determine if the water entering ARS#2 is groundwater from the surrounding area, (i.e. is local groundwater discharging to ARS#2). Based on the depth to water in ARS#2, approximately 7 feet below ground surface (bgs), it was assumed that only shallow monitoring wells would be required to complete this study objective.
Therefore, eight (8) shallow (less than 30 feet bgs) and one (1) deep (approximately 60 feet bgs) wells were installed during the assessment.
One complete round of water level measurements was collected.
Those water level measurements and resulting elevations are shown on Figure 3. Groundwater elevations are also shown on the geologic cross-section included as Figure 5. As indicated, the groundwater elevations are highly variable 3-2 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 particularly in the area of ARS#2. General observations regarding the assessment area groundwater are as follows: " In the area of ARS#l, as characterized by BDL-MW1 through BDL-MW3, groundwater elevations indicate flow to the south toward the topographic low/wetland." In the area of ARS#2, water was detected in BDL-MW5 and BDL-MW6 several days after the wells were installed, however BDL-MW4 remains dry. This indicates that the water observed in BDL-MW5 and BDL-MW6 is not from a local/regional groundwater source.* The water elevation in ARS#2 is higher than that in BDL-MW5 and BDL-MW6 indicating that flow is from the immediate vicinity of ARS#2 to these monitoring wells and not from a local/regional groundwater source.* In the area of ARS#2, groundwater was detected in BDL-MW7 at a significantly lower elevation that the water levels detected in BDL-MW5 and BDL-MW6, indicating that the regional groundwater elevation may be significantly lower than the water level observed in BDL-MW5 and BDL-MW6.* The groundwater elevation at BDL-MW8 was measured to be at or above the ground surface indicating local artesian conditions at this location.* The groundwater elevation at BDL-MW9, which is located approximately 40 feet from the edge of Harris Lake, was measure at an elevation
(-210 feet MSL)approximately 10 feet below the surface water level indicating that surface water from Harris Lake may be discharging to groundwater in this area.3-3 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant April 2009 4
SUMMARY
AND CONCLUSIONS Silar Services Incorporated (SSi) has prepared this Cooling Tower Blowdown Line Assessment Report to document the results of investigation activities performed along a section of the line at the Shearon Harris Nuclear Power Plant, located in New Hill, North Carolina.
The purpose of the assessment was to identify the potential presence and extent of radiological materials in groundwater within the area of the line with respect to the integrity of the line.The Cooling Tower Blowdown Line runs underground for approximately 2 miles from the cooling tower south to the edge of Harris Lake. The line assessment area is located between Air Release System Manhole #1 (ARS#1), which is located adjacent to the composite sampler shed (approximately 0.5 miles from the cooling tower), to ARS#2, located approximately 1,110 feet south of ARS#1. The overall objectives of the Cooling Tower Blowdown Line assessment are as follows:* Characterize the hydrogeology and geology in the area* Provide groundwater sampling and elevation measuring points* Evaluate groundwater flow and groundwater quality" Assess potential sources of tritium concentration in water.<The assessment field activities were completed intwo phases. The first phase included the foll6owing activities:
- Installation of six (6) groundwater monitoring wells BDL-MWl through BDL-MW6 atMpoints along the blowdown line and ARS#2.; <Collection of preliminary groundwater, samples from BDL-MWl; BD-MW2, and BDL-MW-3.," Water level measurements and preliminay groundwater samples from ~BDL-MW5 and BDL-MW6.4-1 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 The scon~d h&&iasfhe aseset included:-Installation of three (3) groundwater monitormg wellsr BDL-MW7. through BDL-MW9at S#2 and toward Harris Lake." Measuirinig water, level elevations." Collecting a complete round of water samples from the mon~itoring wells~ and ARS1#2.1 4.1 Summary of Groundwater Conditions Groundwater samples were collected from the monitoring wells (8 samples) and manhole (1 sample) and analyzed for tritium. Samples from BDL-MW1, BDL-MW5, BDL-MW8, and ARS#2 were also analyzed for zinc, since zinc is added to the cooling water and can be used as a marker analyte. Tritium was detected in five (5) of the eight (8) monitoring wells sampled and in the ARS#2 sample at concentrations up to 2,120 pCi/L. (detected at ARS#2).The highest .concentration of tritium detected in the samples was detected in the immediate area of ARS#2 (ARS#2, BDL-MW5, and BDL-MW6).
The next highest concentration of tritium was detected at BDL-MW3, near the wetland in the area of groundwater discharge.
The highest concentration of zinc was detected in the sample Objective 1.1c ..' RS#2 at a concentration of 187 ug/l.
f transport oftritiated groundwater from the. area near ARS#2 to off-site areas:can be e ated using data collected during this assessment.
>This evaluation assumes tritiated groun dwater is introdtuiced from ARS#2' to~ the environment at a.concentration of approximately 1,260 pji/L (tritium concentration detected in water*samled from located downgradient of ARS#2). Once introduced into they environment tritiatedjgroundwater flows east northeast toward e the.. owner-.controlled area boundary at a rate of ThAppendixD).
The owner-controlled area: boundary in the !general direction of groundwater flow is approximately 1.79 milesj or 9,45 1 feet from the ARS#2 ~area.. Based on these estimates it would take groundwater from the ARS#2 area a~pproximately 49 ~years to ~reachi the 4-2 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 ownter con ITO Iboundary.
Based on Ihec ha If-life of tntiurn (12.3:3 yearstfow rate (193'~ft/year), distancee
(;9,451 eet) inital rtim m:concentration
ýmn te environment!
(1,260 pCi/L) the concentataonkiof tritum in groundwater reaching the. ownercontrol, boudav i.,9 yer ~will have benrdced by approximately forhalf-lives and would be less tthan 80 pCI below the current lower hmit of detecton.t fSupportmg, this analysis is provided in Appendix D, 4.2 Conclusions Based on the occurrence and distribution of tritium in the water samples, it appears that the source of tritium is a leak(s) along the Cooling Tower Blowdown Line. This is based on several observations.
The highest observed tritium concentration was in the sample from the ARS#2 and its immediate vicinity.
The water elevation in ARS#2 is higher than water elevations measured in BDL-MW5 and BDL-MW6, indicating that flow is from the immediate vicinity of ARS#2 to these monitoring wells. In the area of ARS#2, groundwater was detected in BDL-MW7 at a significantly lower elevation than the water levels detected in BDL-MW5 and BDL-MW6, indicating that the regional groundwater elevation may be significantly lower than the water level observed in BDL-MW5 and BDL-MW6. Water was observed to be entering ARS#2 through a pipe that was designed to drain water from the manhole to the surrounding backfill.
It is possible that the backfill surrounding the blowdown line has created a preferential pathway for the flow of water. Water leaking from the pipeline in the vicinity of ARS#2, or at some point in the pipeline at a higher elevation, may be traveling along this preferential "horizontal" pathway as it also infiltrates the surrounding natural material toward the regional water table elevation.
This would create an apparent groundwater mound adjacent to the line in areas where it is above the regional water table.4-3 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 Further investigation is recommended including, but not limited to, the following:
- Evaluation of all manholes in the blowdown line* Installation of sampling points within the blowdown line backfill* Evaluation of the line integrity utilizing video surveillance and or pressure/exfiltration testing.4-4 Cooling Tower Blowdown Line Assessment Report s s .Shearon Harris Nuclear Power Plant Cýý April 2009 FIGURES N Shearon Hanls Nuclear Power Plant eiw Now HIn. NC Quadrangle Location Figurel 0 2000 4000 Feet StSk Loctiko MW Source: U.S.G.S. Topographic Map (7.5 minute)New Hill &: Cokesbury, NC quadrangles SS -Silar Services Inc.
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MSiwumn nm.m Nuamr rwwu rq-x New HI. NC Rq4 Snmy Mach 4, .200 SS. slia Servces imc Lý-
CROSS SECTION LOCATION 100 p .0 in 240 230 220 210 200 190 180 BDL-,' M& DI AM5 6CDL -A A, 0? 41/5W-210 200-190-180 HORIZONTAL SCALE: Fed LEGEND VERTICAL SCALE: _ O'-OVERBURDENGROUNDWA TER ELEVA 77ON WEA THERED SIL TS TONE SCREENED.-. BEDROCK (REGOLITH)
INTERVAL COOLING TOWER BLOWDOWN LINE SILTSTONE BEDROCK Sham Hattis Nuder Pow Plnt Naw H., NC Gfl.am tdcr n-S§ SMar Sevis Dnc-ss.Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 TABLES ss.Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 Table I Monitoring Well Construction Summary Cooling Tower Blowdown Line Assessment Shearon Harris Nuclear Power Plant, New Hill, North Carolina Annular Fill Material Well ID. Well Depth TOC Ground Surface Screen Sand Interval Seal Interval Concrete (bgs) (MSL) Elevation (MSL) Interval (feet (feet bgs) (feet bgs) Interval bgs) (feet bgs)BDL-MW1 30.01 254.68 252.15 30-10 30-5 5-0 NA BDL-MW2 19.34 238.37 236.78 19-9 19-5 5-0 NA BDL-MW3 14.72 224.68 222.88 15-5 15-3 3-0 NA BDL-MW4 17.29 246.96 245.14 17-7 17-5 5-0 NA BDL-MW5 16.64 247.28 245.72 17-7 17-5 5-0 NA BDL-MW6 14.02 247.9 246.12 14-4 14-2.5 2.5-0 NA BDL-MW7 60.94 248.07 245.21 60-30 60-25 25-23 23-0 BDL-MW8 20.33 235.9 233.18 20-10 20-8 8-6 6-0 BDL-MW9 17.87 225.17 222.94 18-8 18-6 6-4 4-0 Notes: bgs -Below Ground Surface TOC -Top of Well Casing MSL -Mean Sea Level NA -Not Applicable Survey data provided by Smith and Smith, accurate to 0.01 feet MSL scS 4 Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 Table 2 Water Level Measurements Cooling Tower Blowdown Line Assessment Shearon Harris Nuclear Power Plant, New Hill, North Carolina Water Level Measurements Location ID Well Depth TOC Ground Surface Depth to Water Northing Easting Latitude Longitude (bgs) (MSL) Elevation (MSL) Water Elevation I _(MSL)ARS#1 683,368.45 2,013,313.56 35037'40 78057'19, NA NA 252.68 NA NA ARS#2 682,311.65 2,012,959.85 35o37'29"'
78057'23' NA NA 247.31 6.75 240.56 BDL-MWI 683,346.51 2,013,326.50 35037'39
78057'18" 30.01 254.68 252.15 23.31 231.37 BDL-MW2 683,128.39 2,013,248.92 35037,37" 78057,19, 19.34 238.37 236.78 11.71 226.66 BDL-MW3 682,926.76 2,013,180.15 35037'35" 78057'20' 14.72 224.68 222.88 4.45 220.23 BDL-MW4 682,319.25 2,012,972.67 35o37,29"'
78o57,23' 17.29 246.96 245.14 DRY NA BDL-MW5 682,300.08 2,012,967.10 35037,29, 78057,23" 16.64 247.28 245.72 8.44 238.84 BDL-MW6 682,308.18 2,012,948.01 35037,29" 78057,23, 14.02 247.9 246.12 7.72 240.18 BDL-MW7 682,308.67 2,012,970.46 35o37'29', 78057,23, 60.94 248.07 245.21 62.93 185.14 BDL-MW8 682,370.85 2,013,154.27 35o37,30
78057'20, 20.33 235.9 233.18 2.05 233.85 BDL-MW9 682,417.76 2,013,249.54 35037'30' 78057'20' 17.87 225.17 222.94 15.2 209.97 Notes: bgs -Below Ground Surface TOC -Top of Well Casing MSL -Mean Sea Level NA -Not Applicable Survey data provided by Smith and Smith SS.Ltl-ýCooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 Table 3 Analytical Results -Water Samples Cooling Tower Blowdown Line Assessment Shearon Harris Nuclear Power Plant, New Hill, North Carolina Sample Tritium Tritium LLD Gamma Analysis
- Zinc Location (pCi/liter) (pCi/liter) (pCi/liter) (ug/1)ARS#2 2,120 233 < LLD 187 BDL-MW1 372 232 *8 BDL-MW2 373 233 BDL-MW3 1,060 232 BDL-MW4 dry BDL-MW5 1,260 233 < LLD 18 BDL-MW6 1,450 232 BDL-MW7 < LLD 234 BDL-MW8 < LLD 232 < LLD 96 BDL-MW9 < LLD 232* The gamma analysis were counted to the Radiological Environmental Program's Lower Limit of Detection (LLD)
SS.CýýCooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 Appendix A Boring Logs 7BORING LOG Drill Rig: Dietrich D-50 Date Drilled: 1/22/09 Logged By: Boring Dia: 6.5 Inches Boring Number: BDL-MW1 Tim Silar a)-a E., //x /Blow lout Comple Counts spoon refusal at 13' bgs 50/4" 50/4" 50/2" F,...............
tion Brn sit w/sm f gr sand 5 10 15 20 25 30-! i I Brn, gry brn sit, mottled Brn, tr gry sit w/ tr cly incresing w/ depth.. ...... Gry f gr sand w/ organic matter.I Bin md-f gr sand Bm/gry cly Rd bm sit w/sm f gr sand Gm gry sit w/cly sm rd bin mottling Weathered rd bin siltstone with tr vf gr ss and tr sh: -Z-Z -. :---------
Depth Feet Lithology Description
~> ~< \Completion Notes: Site: Ground Elevation 252.15 Casing Elevation 254.68 SHNPP Cooling Tower Blowdown Line New Hill, NC Project No.: SHNPP-1 Page 1 4;z BORING LOG Drill Rig: Dietrich D-50 Date Drilled: 1/22/09 Logged By: Boring Dia: 6.5 Inches Boring Number: BDL-MW2 Tim Silar a)-a E M, Blow Counts A// / //~/ \>2>',>K* /7)' /\30 50/2" 26 50/2" 26 50/5" Con npletion------------
Depth Feet Lithology... I ..................
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Brn- It brn t gr sand Rd brn sit 5 10 15 Description M.MM L-- IMM-Weatnerea ra om siltstone f ----------
==I Completion Notes: Site: Ground Elevation 236.78 Casing Elevation 238.37 SHNPP Cooling Tower Blowdown Line New Hill, NC_Project No.: SHNPP-1 Page 1 BORING LOG Drill Rig: Dietrich D-50 Date Drilled: 1/23/09 Logged By: Boring Dia: 6.5 Inches Boring Number: BDL-MW3 Tim Silar E (I)Blow lout Comple Counts 40 50/4" 36 50/3.5"/Y: ::Y.................
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BEn sity t gr sand, sm mottling Depth Feet I- ..-5 M -.71-:':'--'L-1:-----:-'-
Lithology Highly weathered rd brn siltstone Weathered rd bm siltstone, good water zone @ -10.5' bgs Description 6 --------------
A 10-15 Completion Notes: Site: Ground Elevation 222.88 Casing Elevation 224.68 SHNPP Cooling Tower Blowdown LinE New Hill, NC Project No.: SHNPP-1 Page 1 BORING LOG Drill Rig: Dietrich D-50 Date Drilled: 1/23/09 Logged By: Boring Dia: 6.5 Inches Boring Number: BDL-MW4 Tim Silar E C,)7/7 Blow lout Comple Counts tion 16 50/4" 38 50/2" 50/4.5" 30 50/2" 36 50/4" tion Brn sit w/f gr sand, organic matter Rd brn w/ sm gry sit w/sm siltsone, possible fill................ "I',,',',, ",,, "I'll" I'll .. .1-5-10 -..................
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Weathered rd brn siltstone, sm gry siltstone, dry Depth Lithology Feet Description
,..,+ -15 4 Completion Notes: Site: Ground Elevation 245.14 Casing Elevation 246.96 SHNPP Cooling Tower Blowdown Line New Hill, NC Project No.: SHNPP-1 Page 1 BORING LOG Drill Rig: Dietrich D-50 Date Drilled: 1/26/09 Logged By: Boring Dia: 6.5 Inches Boring Number: BDL-MW5 Tim Silar E CU (IX 77 -Blow Counts 50/4" 36 50/5" 50/4" Comple tion Depth Feet Lithology"1 Brn with sm gry sit w/ sm cly, tr f gr sand, dense, dry 5 -10 Description
Weathered rd brn siltstone, sm gry siltstone, dry 15-~=- =~Completion Notes: Site: Ground Elevation 245.72 Casing Elevation 247.28 SHNPP Cooling Tower Blowdown Line New Hill, NC Project No.: SHNPP-1 Page 1 BORING LOG Drill Rig: Dietrich D-50 Date Drilled: 1/27/09 Logged By: Boring Dia: 6.5 Inches Boring Number: BDL-MW6 Tim Silar a)'a E (I)x /V V Blow Counts Completion Depth Feet Lithology Description 4-- -- ~..---, 4 -Brn with sm rd brn sit w/ tr cly and vf gr sand, tr organic matter L=18 26 50/5" 26 50/5" 30 50/3" 20 40 50/3" 30 50/4" 5 Weathered rd brn siltstone, sm gry siltstone, dry 4--15 -Completion Notes: Site: Ground Elevation 246.12 Casing Elevation 247.90 SHNPP Cooling Tower Blowdown LinE New Hill, NC Project No.: SHNPP-1 Page 1 BORING LOG Drill Rig: Geoprobe Date Drilled: 2/17/09 Logged By: Boring Dia: 4 Inches Boring Number: BDL-MW7 Tim Silar-~Blow Depth Lihog BCou Completion e Lithology Description aE Counts Feet-U)O a. 4* S S a I S a a a*0 a a a a 5 10 15 20 25 30 35 40 45 50 55--------------
71 -.. 7' 7. 7 t I L I M. M -1 M., Brn with sm rd bm sit w/tr cly and vf gr sand, tr organic matter Weathered rd brn siltstone, sm gry siltstone, dry..... ......Siltstone 60.1 Completion Notes: Site: Ground Elevation 245.21 Casing Elevation 248.07, Solid stem SHNPP Cooling Tower Blowdown LinE augers to -17' bgs with air rotary from 60' bgs New Hill, NC Project No.: SHNPP-1 Page 1 BORING LOG Drill Rig: Geoprobe Date Drilled: 2/17/09 Logged By: Boring Dia: 4 Inches Boring Number: BDL-MW8 Tim Silar'a Blow Completion Depth Lithology Description E Counts Feet a a'.a a a* a'4'a Brn with sm rd brn sit w/ tr cly and vf gr sand, tr organic matter 5 10 20----------------
Weathered rd brn siltstone, sm gry siltstone, dry ký ----------------
I Siltstone, water zone at 14-15' bgs Completion Notes: Site: Ground Elevation 233.18 Casing Elevation 235.90, Solid stem SHNPP Cooling Tower Blowdown Line augers to -12' bgs with air rotary from 20' bgs New Hill, NC Project No.: SHNPP-1 Page 1 BORING LOG Drill Rig: Geoprobe Date Drilled: 2/17/09 Logged By: Boring Dia: 4 Inches Boring Number: BDL-MW9 Tim Silar S Blow Completion Depth Lithology Description E Counts Feet C,, a a U a a Brn and gry cly sit-5-10 -i Grysit Rd brn siltstone, dry Completion Notes: Site: Ground Elevation 222.94 Casing Elevation 225.17, Solid stem SHNPP Cooling Tower Blowdown Line augers to -8' bgs with air rotary 18' bgs New Hill, NC_Project No.: SHNPP-1 Page 1 ss.Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 Appendix B NCDENR Well Construction Records NON RESIDENTIAL WELL CONSTRUCTION RECORD North Carolina Department of Environment and Natural Resources-Division of Water Quality WELL CONTRACTOR CERTIFICATION
- 2402 I. WELL CONTRACTOR:
MIKE MCCONAHEY Well Contractor (Individual)
Name GEOLOGIC EXPLORATION, INC, Well Contractor Company Name STREET ADDRESS 176 COMMERCE BLVD STATESVILLE NC 28625 City or Town State Zip Code 704 -872-7686 Area code- Phone number 2. WELL INFORMATION:
SITE WELL ID#(if applicable)
BDL-MW-1 STATE WELL PERMIT#(if applicable)_
DWQ or OTHER PERMIT #*lf applicable)
WELL USE (Check Applicable Box) Monitoring 9] Municipal/Public 0 Industrial/Commercial
[3 Agricultural
[I Recovery D Injection 0 IrrigationC3 Other 0 (list use)DATE DRILLED 01/22/09 TIME COMPLETED
-AMO PMQ 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbera, Community, Subdivision, Lot No., Parcel, Zip Code)TOPOGRAPHIC
/ LAND SETTING: 0 Slope OValley []Flat ORidge 0 Other (check appropriate box)LATITUDE be in degres, Sminutes, seconds or LONGITUDE in a decimal format Latitude/longitude source: oGPS oTopographic map (location of we# must be shown on a USGS topo map and attached to this form Inot ushig GPS)4. FACILITY-is the nnme of fe business where the well is wlat.FACILITY ID #(if applicable)_
NAME OF FACILITY SHEARON HARRIS NUCLEAR PLANT STREET ADDRESS SHEARON HARRIS ROAD NEW HILL NC 27562 d. TOP OF CASING IS 0.0 FT. Above Land Surface"Top of casing terminated at/or below land surface may require a variance in accordance with 15A NCAC 2C .0118.e. YIELD (gpm): N/A METHOD OF TEST N/A f. DISINFECTION:
Type N/A Amount N/A g. WATER ZONES (depth): From To__ From___ To From__ To_ From___ To From -To_ From___ To 6. CASING: Thickness/
Depth It W~hS W4~ral Fro_ _ To 10.0 ____ __Frm.0 Dpt Ft._2~1 __ ___From To Ft.From__ To_ FLt 7. GROUT: Depth Material Method From To Ft.From " To Ft_From -To Ft.8, SCREEN: Depth Diameter Slot Size Material From 10.0 To 30.0 Ft 2.0 in. .010 in, PVC From__ To Ft. in. _ in __From _ To__ FL in. In.9. SAND/GRAVEL PACK: Depth Size Material From. 5.0 To 30.0 Ft 20-40 FINE SILICA SAND From. To FtL_From To Ft._10. DRILLING LOG From To Formation Description 0.0 1.0 GRASS/TOPSOIL 1.0 14.0 ORANGEr/AN/WHITE SANDY CLAYEY SILT 14.0 30.0 BROWN/RED SANDY SILT City or Town State Zip Code CONTACT PERSON PROGRESS ENERGY MAILING ADDRESS PO BOX 10429 SOUTHPORT NC 28419 City or Town State. Zip Code Area code -Phone number 5. WELL DETAILS: a. TOTAL DEPTH: 30.0 FEET b. DOES WELL REPLACE EXISTING WELL? YES 0. NO E)c. WATER LEVEL Below Top of Casing: 0.0 (DRY) FT.(Use "" If Above Top of Casing)11. REMARKS: BENTONrTE SEAL FROM 0.0 TO 5.0 FEET I I MIKE MCCONAHEY PRINTED NAME OF PERSON CONSTRUCTING THE WELL Submit the original to the Division of Water Quality within 30 days. Attn: Information Mgt., 11617 Mail Service Center- Raleigh, NC 27699-1617 Phone No. (919) 733-7015 ext 568.Form GW-lb Rev. 7/05 NONRESIDENTIAL WELL CONSTRUCTION RECORD North Carolina Department of Environment and Natural Resources-Division of Water Quality WELL CONTRACTOR CERTIFICATION
- 2402 1. WELL CONTRACTOR:
MIKE MCCONAHEY Well Contractor (Individual)
Name GEOLOGIC EXPLORATION, INC.Well Contractor Company Name STREET ADDRESS 176 COMMERCE BLVD STATESVILLE NC 28625 City or Town State Zip Code (704 -872-7686 Area code- Phone number 2. WELL INFORMATION:
SITE WELL.ID #(if applicable)_
BDL-MW-2 STATE WELL PERMIT#(if applicable)
DWO or OTHER PERMIT #(if applicable)_
WELL USE (Check Applicable Box) Monitoring
- 8) Municipal/Public
[I Industrial/Commerciai 0 Agricultural 0 Recovery 0] Injection
[0 Irrigationo Other 0 (list use)__ _DATE DRILLED 0117.2./09 TIME COMPLETED AM n PM r 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbers, Community, Subdfivsion, Lot No., Parcel, Zip Code)TOPOGRAPHIC
/ LAND SETTING: OSIope OValley 0Flat []Ridge 0 Other (check appropriate box)LATITUDE _ May be in degrees, minutes, seconds or LONGITUDE in a decimal format Latitude/longitude source: oGPS oTopographic map'(location of wel must be shown on e USGS topo map and attached to this form if not using GPS)4. FACIUTY. Is the name of the business where the well Is located.FACILITY ID #(if applicable)
NAME OF FACIUTY SHEARON HARRIS NUCLEAR PLANT STREET ADDRESS SHEARON HARRIS ROAD NEW HILL NC 27562 d. TOP OF CASING IS 0.0 FT. Above Land Surface**Top of casing terminated at/or below land surface may require a variance In accordance with 15A NCAC 2C .0118.e. YIELD (gpm): N/A METHOD OF TEST N/A f. DISINFECTION:
Type N/A .Amount N/A g. WATER ZONES (depth): From -To -From To From To_ _ From To From _ To From To 6. CASING: Thickness/
Depth Da From 0.0 To 4, 0 Ft._2 1 IrCt From To Ft From _ To_ Ft._7. GROUT: Depth Material Method From To Ft.From _ To Ft Fromr___ To_ Ft.8. SCREEN: Depth Diameter Slot Size Material From 4.0 To 19.0 Ft. 2.0 in. .010 In. PVC From To Ft. in. in.From _ To_ _ Ft.- in. 'tn.9. SANDIGRAVEL PACK: Depth Size Material From 2.0 To 19.0 Ft. 20-40 FINE SILICA SAND From To_ _ Ft.From T.__T___ Ft.10. DRILLING LOG From To Formation Description 0.0 1.0 GRASS/TOPSOIL 1.0 10.0 ORANGE/TAN/WHITE SANDY CLAYEY SILT 10.0 19.0 BROWN/RED SANDY SILT 11. REMARKS: BENTONITE SEAL FROM 0.0 TO 2.0 FEET City or Town State Zip Code CONTACT PERSON PROGRESS ENERGY MAIUNG ADDRESS PO BOX 10429 SOUTHPORT NC 28419 City or Town State Zip Code Area code -Phone number 5 WELL DETAILS: a. TOTAL DEPTH: 19.0 FEET b. DOES WELL REPLACE EXISTING WELL? YES O NO El c. WATER LEVEL Below Top of Casing: 0.0 (DRY) FT.(Use "+" if Above Top of Casing)I Y TFY THAT THIS WELL WA;S CO ' 'STR *LITD IN ACCORDANCE WITH A TANQR DS, AND THAT A COPY OF THIS S 02/24/09 0 1 .SIGNATURE CP'CERTIFIED WELL C5ý "TOR MIKE MCCONAHEY DATE PRINTED NAME OF PERSON CONSTRUCTING THE WELL Submit the original to the Division of Water Quality within 30 days. Attn: Information Mgt., 1617 Mail Service Center- Raleigh, NC 27699-1617 Phone No. (919)733-7015 ext 568.Form GW-lb Rev. 7105 NON RESIDENTIAL WELL CONSTRUCTION RECORD North Carolina Department of Environment and Natural Resources-Division of Water Quality WELL CONTRACTOR CERTIFICATION
- 2402 1. WELL CONTRACTOR:
MIKE MCCONAHEY Well Contractor (Individual)
Name GEOLOGIC EXPLORATION, INC.Well Cortractor Company Name STREET ADDRESS 176 COMMERCE BLVD STATESVILLE NC 28625 City or Towm State Zip Code (704 .872-7686 Area code- Phone number 2. WELL INFORMATION:
SITE WELL ID #(it applicable)
BDL-MW-3 STATE WELL PERMIT#QT applicable)_
DWO or OTHER PERMIT #(if applicable)
WELL USE (Check Applicable Box) Monitoring E3 MunicipalP/iloic 0 IndustriallCommercial 0" Agricultural 0 Recovery 0 Injection 0]Irrigationo Other 0 (list use)DATE DRILLED 01/23/09 TIME COMPLETED AM E] PMQ 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbers, Community, Subdivision, Lot No., Parcel, Zip Code)TOPOGRAPHIC
/ LAND SETTING: 0Slope OVdley OFlat oRidge o Other (check appropriate box)LATITUDE -_____ May be in degreezs, minutes, seconds or LONGITUDE in a decimal format Latitude/longitude source: OGPS oTopographic map (locatibn of welI must be shown on a USGS topo map and attached to this form if not using GPS)4. FACILITY-is tie nnae a the business where the well Is located.FACILITY ID #(#f applicable)_
NAME OF FACILITY SHEARON HARRIS NUCLEAR PLANT STREET ADDRESS SHEARON HARRIS ROAD NEW HILL NC 27562 d. TOP OF CASING IS 0.0 FT. Above Land Surface**Top of casing terrrinated at/or below land surface may require a variance in accordance with 15A NCAC 2C .0118.e. YIELD (gpm): NIA METHOD OF TEST N/A I. DISINFECTION:
Type N/A Amount N/A g. WATER ZONES (depth): From -To From To From To _ From -To From To_ From_ To 6. CASING: Thickness/
Depth Djamfe Matria From 0.0 To 5.0 FL 2 I PV From_ _ To Ft._From To Ft._7. GROUT: Depth Material Method From_ _ To Ft.From To FL From -To_ Ft 8. SCREEN: Depth Diameter Slot Size Material From 5.0 To_15.0 FL 2.0 in..010 In. PVC From To_ Ft. in. in.From- To__ Ft _ in. in.9. SANDIGRAVEL PACK: Depth Size Material From 3.0 To 15.0 Ft. 20-40 FINE SILICA SAND From To FL_From To Ft._10. DRILLING LOG From To Formation Description 0.0 1.0 GRASSrTOPSOIL 1.0 6.0 ORANGE/TAN/WHITE SANDY CLAYEY SILT 6,0 15.0 BROWN/RED SANDY SILT City or Town State Zip Code CONTACT PERSON PROGRESS ENERGY MAILING ADDRESS PO BOX 10429 SOUTHPORT NC 28419 11. REMARKS: BENTONITE SEAL FROM 0.0 TO 3.0 FEET City or Town State Zip Code Area code -Phone number 5. WELL DETAILS: a. TOTAL DEPTH: 15.0 FEET b. DOES WELL REPLACE EXISTING WELL? YES 0 NO 91 c. WATER LEVEL Below Top of Casing: 0.0 (DRY) FT.(Use +" if Above Top of Casing)THIS WELL WAS CONSTRUCTED IN ACCORDANCE WfTH rRU'II SThAIDARDS, AND THAT A COPY OF THIS 02/24109 SIGNATURE
&F CERTIFIED WELL MIKE MCCONAHEY DATE PRINTED NAME OF PERSON CONSTRUCTING THE WELL Submit the original to the Division of Water Quality within 30 days. Attn: Information Mgt., 1617 Mail Service Center- Raleigh, NC 27699-1617 Phone No. (919) 733-7015 ext 568.Form GW-lb Rev. 7/05 NONRESIDENTIAL WELL CONSTRUCTION RECORD North Carolina Department of Environment and Natural Resources-Division of Water Quality WELL CONTRACTOR CERTIFICATION
- 2402 1. WELL CONTRACTOR:
MIKE MCCONAHEY Well Contractor (Individual)
Name GEOLOGIC EXPLORATION, INC.Well Contractor Company Name STREET ADDRESS 176 COMMERCE BLVD STATESVILLE NC 28625 City or Town State Zip Code 704 872-7686 Area code- Phone number 2. WELL INFORMATION:
SITE WELL ID #Nif aplicable)
BDL-MW-4 STATE WELL PERMIT#C'i applicable)_
DWQ or OTHER PERMIT #(if applicable)
_ ....._.WELL USE (Check Applicable Box) Monitoring 01 Municipal/Public D IndustzlaVCorrmerciad
] Agrlcultural 0 Recoveryo Injection 0 Irrgationo Other 0 (list use)DATE DRILLED 01/23/09 TIME COMPLETED AM O PM O 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbers, Community, Subdiision.
Lot No., Parcel, Zip Code)TOPOGRAPHIC
/ LAND SETTING:[]Slope [3Valley 0 Fat -Ridge E] Other (check appropriate box)LATITUDE -May be in degrees.minutes, seconds or LONGITUDE in a decimal format Latitude/longitude source: oGPS oTopographic map (kcation of we# must be shown on a USGS topo map and attached to this form if not using GPS)4. FACIUTY- Is the name of the business where Vie wet im loceted.FACILITY ID #(if applicable)
NAME OF FACILITY SHEARON HARRIS NUCLEAR PLANT STREET ADDRESS SHEARON HARRIS ROAD NEW HILL NC 27562 d. TOP OF CASING IS 0.0 FT. Above Land Surface**Top of casing terminated at/or below land surface may require a variance in accordance with 15A NCAC 2C .0118.e. YIELD (gpm): N/A METHOD OF TEST N/A f. DISINFECTION:
Type N/A Amount N/A g. WATER ZONES (depth): From ~ To From__ To___From___ To_ From To From ___ To _ FronT To_6. CASING: Thickness/
-Depth Dow ameter ~ ateia From___..
.2% I~cHvc~) Matei From 0.0 To 7.5 FL From To Ft._From To Ft.7. GROUT: Depth Material Method From_ To__ Ft From To Ft.From To_____ Ft.8. SCREEN: Depth Diameter Slot Size Material From 7.5 To 17.5 Ft. 2.0 in. .010 in. PVC From To Ft. In. in.From____ To Ft in. _ in.9. SANDIGRAVEL PACK: Depth Size Material From 5.0 To 17.5 Ft. 20-40 FINE SILICA SAND From To__ Ft._From To Ft._10. DRILLING LOG From To Formation Description 0.0 1.0 GRASS/TOPSOIL 1.0 6.0 ORANGEITANtWHITE SANDY CLAYEY SILT 6.0 17.5 BROWN/RED SANDY SILT 11. REMARKS: BENTONITE SEAL FROM 0.0 TO 5.0 FEET City or Tovn State Zip Code CONTACT PERSON PROGRESS ENERGY MAILING ADDRESS P0 BOX 10429 SOUTHPORT NC 28419 City or Town State Zip Code Area code -Phone number 5. WELL DETAILS: a. TOTAL DEPTH: 17.5 FEET b. DOES WELL REPLACE EXISTING WELL? YES 0 NO !]c. WATER LEVEL Below Top of Casing: 0.0(DRY) FT.(Use "+ If Above Top of Casing)too AA.Y CERTIFY THAT THIS WELL WAS CONSiRUCOTE IN ACCORDANCE WITH 1 5~C 2C,..LL CONSTRUCTION STANDARDS, AND THAT A COPY OF THIS Is~r H~ EN PRV9ý qjW R SIGNATURE O ?.CERTIFIED WELL CO OR DATE MIKE MCCONAHEY PRINTED NAME OF PERSON CONSTRUCTING THE WELL Submit the original to the Division of Water Quality within 30 days. Attn: Information Mgt., 1617 Mall Service Center- Raleigh, NC 27699-1617 Phone No. (919) 733-7015 ext 568.Form GW-lb Rev. 7/05 NONRESIDENTIAL WELL CONSTRUCTION RECORD North Carolina Department of Environment and Natural Resources-Division of Water Quality WELL CONTRACTOR CERTIFICATION
- 3214 1. WELL CONTRACTOR:
RANDY OWNBEY Wdll Contractor (Indivdual)
Name GEOLOGIC EXPLORATION, INC.Well Contractor Company Name STREET ADDRESS 176 COMMERCE BLVD STATESVILLE NC 28625 City or Town State Zip Code 7 872-7686 Area code- Phone number 2. WELL INFORMATION:
SITE WELL ID #(if appficabie)_
BDL-MW-5 STATE WELL PERMIT#(if applicable)
_ _ _DWQ or OTHER PERMIT #(if applicable)_
WELL USE (Check Applicable Box) Monitoring
[J MunicipaV/Public
[I Industrial/Commercial 0 Agricultural
[I Recovery[)
Irjection D Irrigationo Other C (list use)DATE DRILLED 01127/09 TIME COMPLETED AM 0 PM 0 3. WELL LOCATION: CITY: NEW HILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbers, Community, Subdhision, Lot No., Parcel, Zip Code)TOPOGRAPHIC
/ LAND SETTING:[I Slope DValley [ Flat 0JRidge O Other (check appropriate box)LATITUDE _____t__,May be in degrees.minutes. seconds or LONGITUDE in a decimal format Latitude/longitude source: oGPS oTopographic map (location of well must be shown on a USGS topo map and attached to this form if not using GPS)4. FACILITY-Is the name or the business where te well is located.FACILITY ID #(df applicable)
NAME OF FACIUTY SHEARON HARRIS NUCLEAR PLANT STREET ADDRESS SHEARON HARRIS ROAD NEW HILL NC 27562 d. TOP OF CASING IS 0.0 FT. Above Land Surface**Top of casing terminated at/or below land surface may require a variance in accordance with 15A NCAC 2C .01 18.a. YIELD (gpm): NIA METHOD OF TEST N/A f. DISINFECTION:
Type N/A Amount N/A g. WATER ZONES (depth): From_ _ __To From To__From____ To_ From_ __ To Front_ To From_. To____6. CASING: Thickness/
Depth F1ilarter Mateal From 0.0 To 7.0 FL_2 NGH PVC From_ To_ Ft._From___ To__ FL _7. GROUT: Depth. Material Method From -To Ft.From _ To _ FL_From___ To _ Ft.8. SCREEN: Depth Diameter Slat Size Material From 7.0 To 17.0 FL 2.0 in. .010 In. PVC From_ _ To Ft. in. In.From___ To____ Ft. in. in.9. SANDIGRAVEL PACK: Depth Size Material From 5.0 To 17.0 Ft. 20-40 FINE SILICA SAND From To Ft.From __ To Ft.___10. DRILUNG LOG From To Formation Description 0.0 1.0 GRASS/TOPSOIL 1.0 6,0 ORANGE/TAN/WHITE SANDY CLAYEY SILT 6-0 17.0 BROWN/RED FINE SANDY SILT 11. REMARKS: BENTONITE SEAL FROM 0.0 TO 5.0 FEET City or Town State Zip Code CONTACT PERSON PROGRESS ENERGY MAILING ADDRESS P0 BOX 10429 SOUTHPORT NC 28419 City or Town State Zip Code Area code -Phone number 5. WELL DETAILS: a. TOTAL DEPTH: 17.0 FEET b. DOES WELL REPLACE EXISTING WELL? YES [I NO 9J c. WATER LEVEL Below Top of Casing: 0.0 (DRY) FT.(Use "+* if Above Top of Casing)I DO HEREBY CERTIFY THAT THIS WELL WAS CONSTRUCTED IN ACCORDANCE WITH 15A NCAC 2C, WELL CON U U)ON STANDARDS, AND THAT A COPY OF THIS ENz PI TO THE WELL OWNER.
CER'fIED WELL CONTRACTOR RANDY OWNBEY DATE PRINTED NAME OF PERSON CONSTRUCTING THE WELL Submit the original to the Division of Water Quality within 30 days. Attn: Information Mgt., 1617 Mall Service Center- Raleigh, NC 27699-1617 Phone No. (919) 733-7015 ext 568.Form GW-lb Rev. 7/05
"'4~, fl~'NONRESIDENTIAL WELL CONSTRUCTION RECORD North Carolina Department of Environment and Natural Resources-Division of Water Quality WELL CONTRACTOR CERTIFICATION
- 3214 1. WELL CONTRACTOR:
RANDY OWNBEY Well Contractor (Individual)
Name GEOLOGIC EXPLORATION, INC.Well Contractor Company Name STREET ADDRESS 176 COMMERCE BLVD STATESVILLE NC 28625 City or Town State Zip Code (74 y872-7686 Area code- Phone number 2. WELL INFORMATION:
SITE WELL ID #(If applicable)
BDL-MW-6 STATE WELL PERMIT#Vf applicable).
DWQ or OTHER PERMIT #(if applicable)_
_ _WELL USE (Check Applicable Box) Monitoring gj Municipal/Public 0 Industrial/Commercial 0 Agricultural 0 Recovery [I Injection 0 IrrigationD Other 0 (ist use)DATE DRILLED 01126/09 TIME COMPLETED AMO PMO 3. WELL LOCATION: CITY: NEWHILL COUNTY WAKE SHEARON HARRIS ROAD 27562 (Street Name, Numbers, Community, Subdivision, Lot No., Parcel, Zip Code)TOPOGRAPHIC I LAND SETTING: OSIope OValley -]OFat 0 Ridge -] Other (check appropriate box)LATITUDE ____utMay be in degrees, minutes, seconds or LONGITUDE in a decimal format Latitude/longitude source: OGPS oTopographic map (location of we/ must be shown on a USGS topo map and attached to this form if not uskig GPS)4. FACIUTY- is the name of the business where the well is located.FACIUTY ID #(if applicable)_
NAME OF FACILITY SHEARON HARRIS NUCLEAR PLANT STREET ADDRESS SHEARON HARRIS ROAD NEW HILL NC 27562 City or Towni State Zip Code CONTACT PERSON PROGRESS ENERGY MAILING ADDRESS PO BOX 10429 SOUTHPORT NC 28419 City or Town State Zip Code Area code -Phone number S. WELL DETAILS: a. TOTAL DEPTH: 14.0 FEET b. DOES WELL REPLACE EXISTING WELL? YES 0 NO Ej c. WATER LEVEL Below Top of Casing: 0.0 (DRY) FT.(Use "+" if Above Top of Casing)d. TOP OF CASING IS 0.0 FT. Above Land Surface**Top of casing terminated at/or below land surface may reqLire a variance in accordance with ISA NCAC 2C .0118.e. YIELD (gpm): N/A METHOD OF TEST N/A f. DISINFECTION:
Type N/A Amount NlA g. WATER ZONES (depth): From To From To From__ To _ From -To From -To_ From To 6. CASING:, Thickness/
Depth Diareer %VW ht P Material From 0.0 To 4.0 Ft._2N PVC From -To_ Ft._From _ To__ Ft._7. GROUT: Depth Material Method From -To_ Ft.From -To : Ft From -To_ FL 8. SCREEN: Depth Diameter , Slot Size Material From 4.0 To 14.0 Ft. 2.0 in. .010 In. PVC From _ To _ Ft. In. in.From__ _ To _ Ft. in. in.9. SAND/GRAVEL PACK: Depth Size Material From 2.0 To 14.0 Ft. 20-40 FINE SILICA SAND From To Ft. _From To Ft._M0. DRILUNG LOG From To Formation Description 0.0 1.0 GRASS/TOPSOIL 1.0 6.0 ORANGE/TAN/WHITE SANDY CLAYEY SILT 6.0 14.0 BROWN/RED FINE SANDY SILT 11. REMARKS: BENTONITE SEAL FROM 0.0 TO 2.0 FEET I DO HEREBY CERTIFY THAT THIS WELL WAS CONSTRUCTED IN ACCORDANCE WITH 15A NCAC 2C. WELL qNS RUCTION STANDARDS.
AND THAT A COPY OF THIS TO THE WELL OWNER./V 1//02/26/09 SIGN.9UIP OF CEKI-IFIED WELL CONTRACTOR RANDY OWNBEY DATE PRINTED NAME OF PERSON CONSTRUCTING THE WELL Submit the original to the Division of Water Quality within 30 days. Attn: Information Mgt., 1617 Mail Service Center- Raleigh, NC 27699-1617 Phone No. (919)733-7015 ext 568.Form GW-lb Rev. 7/05 NONRESIDENTIAL WELL CONSTRUCTION RECORD North Carolina Department of Environment and Natural Resources Division of Water Quality WELL CONTRACTOR CERTIFICATION
- 3106 1. WELL CONTRACTOR:
James 0. Barker Well Contractor (Individual)
Name Quantex, Inc.Well Contractor Company Name STREET ADDRESS P.O. Box 41673 Raleigh, NC 27629 City or Town State Zip Code 9 219 -9604 Area code- Phone number 2. WELL INFORMATION:
SITE WELL ID#Qfrappllcable)
NA -a.WELL CONSTRUCTION PERMIT#(if applicable)
NA OTHER ASSOCIATED PERMIT #(if applicable)
NA 3. WELL USE (Check Applicable Box) Monitonnge Municipal/Publicz Industrial/CommercialD Agriculturaln Recovery[]
Injection[]
Irnigatlorfj OtherO (list use)DATE DRILLED 2/17/09 TIME COMPLETED J ... AMR PME]4. WELL LOCATION: CITY: New Hill COUNTY Wake New Hill Holleman Road, New Hill, NC 27562 (Street Name. Numbers, Community, Subdivision, Lot No., Parcel. Zip Code)TOPOGRAPHIC
/ LAND SETTING: R Slope n Valley 13 Flat G Ridge 13 Other (check appropriate box) May be in degrees, LATITUDE N35 deg. 37.024' minutes. seconds or LONGITUDE W!78 deg. 57.606' in adecimal format Latitude/longitude source: 4 GPS 0 Topographic map (location of well must be shown on a USGS topo map and attached to this form if not using GPS)5. FACIUTY. is tme nane of the business vwwere me ie Is bocatd.FACILITY ID #(if applicable)
NA NAME OF FACILITY Progress Enemy Shearon H. Plant STREET ADDRESS New Hill Holleman Road New Hill NC 27562 d. TOP OF CASING IS 2.5' FT. Above Land Surface**Top of casing terminated at/or below land surface may require a variance in accordance with 15A NCAC 2C .0118.e. YIELD (gpm): NA METHOD OF TEST NA f. DISINFECTION:
Type NA Amount NA g. WATER ZONES (depth): From 40A To 5o' From To From To From__ To From To From To 7. CASING: Depth Diameter ThicknessNVeight Material From_.0__
To_____ Ft 2- sch40 PVC From To _ Ft._From To Ft 8. GROUT: I Depth Material Method From 0 To 24'9 FL Neat Cement Pour Fromi _L FL Bentonite Place From _ To._ FtL 9. SCREEN: I Depth Diameter Slot Size Material From_ -To 0(, FL 2* in. 0.010 in. PVC From -To Ft. in. in.From_ To _ Ft. in. in.10. SANDIGRAVEL PACK: Depth i £ Size Material From 0,6 To Ft. #2 Silica Sand From To_ Ft._From To_ Ft._11.DRILLING LOG From To Formation Description
- 12. REMARKS:_A A 2c. , 2 i, C TION STANDARDS.
AND THAT A COPY F THI HAS PVVJJ TO THE WELL OWNER.SK TU OF CERTIFIED WELL CONTRACTOR iATE Ja es D. Barker PRINTED NAME OF PERSON CONSTRUCTING THE WELL City or Town State Zip Code CONTACT PERSON Tim Silar MAILING ADDRESS New Hill Holleman Road New Hill NC 27562 City or Town State Zip Code NA Area code -Phone number 6. WELL DETAILS: a. TOTAL DEPTH: L-0 b. DOES WELL REPLACE EXISTING WELL? YESO NOR c. WATER LEVEL Below Top of Casing: NA FT.(Use "+" if Above Top of Casing)Submit the original to the Division of Water Quality within 30 days. Attn: Information Mgt., 1617 Mail Service Center- Raleigh, NC 27699-1617 Phone No. (919) 733-7015 ext 568.Form GW-1b Rev.12107 A .A~ ...if~J7~ I, N ,ON RESIDENTIAL WELL CONSTRUCTION RECORD North Carolina Department of Environment and Natural Resources Division of Water Quality WELL CONTRACTOR CERTIFICATION
- 3106 1. WELL CONTRACTOR:
James D. Barker Well Contractor (Individual)
Name Quantex, Inc.Well Contractor Company Name STREETADDRESS P.O. Box 41673 Raleigh, NC 27629 City or Town State Zip Code 91 2 1 9-9604 Area code- Phone number 2. WELL INFORMATION:
SITE WELL 10 #(ifapplicable)
A9W " L-r MW' -q WELL CONSTRUCTION PERMIT#(ifapplicable)
NA OTHER ASSOCIATED PERMIT #(if applicable)
NA 3. WELL USE (Check Applicable Box) Monitoringo MunlcipaV/Publlcl Industrlal/Commercial AgrlculturalO Recovery[]
Injectionl3 Irmgatiorfl OtherD) (list use)DATE DRILLED 2117109 TIME COMPLETED 2 AM13s PM 4. WELL LOCATION: CITY: New Hill COUNTY Wake New Hill Holleman Road, New Hill, NC 27562 (Street Name. Numbers, Community, Subdivision, Lot No.. Parcel, Zip Code)TOPOGRAPHIC
/ LAND SETTING: N Slope 11 Valley [] Flat a Ridge El Other (check appropriate box) May be in degrees, LATITUDE N35 deg. 37.024' minutes, seconds or LONGITUDE W78 deg. 57.606' in a decimal format Latitude/longitude source: & GPS [] Topographic map (location of well must be shown on a USGS topo map and attached to this form if not using GPS)5. FACIUITY.
is the name of the busiress where the wel Is located.FACILITY ID #(if applicable)
NA NAME OF FACILITY Progress Energy Shearon H. Plant STREET ADDRESS New Hill Holleman Road New Hill NC 27562 d. TOP OF CASING iS 2.5' FT. Above Land Surface**Top of casing terminated at/or below land surface may require a variance in accordance with 15A NCAC 2C .0118.a. YIELD (gpm): NA METHOD OF TEST NA f. DISINFECTION:
Type NA Amount NA g. WATER ZOIqES (depth): From 17 To_ _ From To From -To__-___ From- To From_ _ To From TO 7. CASING: i Depth , I Diameter Thickness/Weight Material FromQ.) To tO Ft. 2" sch4O PVC From To_ Ft.From To_ FL.8. GROUT: Depth Material Method Fro 6 To _ _ Ft Neat Cement Pour FromZZ0 To-..:ii Ft. Bentonite Place From To Ft.9. SCREEN: ( Depth ( Diameter Slot Size Material From dO To 2L) Ft 2" in. 0.010 in. PVC From _ To _ Ft. in. _ in. __From _ To_ _ Ft. in. in.10. SANDIGRAVEL PACK: Depth I e Size Material From58 To 20 Ft. #2 Silica Sand Fromn To_ Ft.From To_ Ft.I11DRILWNG LOG From To Formation Description 1 R 12. REMARKS: City or Town State Zip Code CONTACT PERSON Tim Silar MAILING ADDRESS New Hill Holleman Road New Hill NC 27562 City or Town State Zip Code ( ). NA Area code -Phone number 6. WELL DETAILS: (a. TOTAL DEPTH:_ ____b. DOES WELL REPLACE EXISTING WELL? YES13 NOB c. WATER LEVEL Below Top of Casing: NA FT, (Use "+"if Above Top of Casing)I W FYT T S WELL WAS CONSTRUCTED IN ACCORDANCE WITHC. VL CO4 t ION STANDARDS, AND THAT A COPY OFTIIS.AS ralý-l P EqF TOHEWEU. OWNER /T kTLURE 4F CERTIFIED WELL CONTRACTOR
'DA11E Ja es D. Barker PRINTED NAME OF PERSON CONSTRUCTING THE WELL Submit the original to the Division of Water Quality within 30 days. Attn: Information Mgt., 1617 Mail Service Center- Raleigh, NC 27699-1617 Phone No. (919) 733-7015 ext 568.Form GW-lb Rev. 12/07 NON RESIDENTLIL WELL CONSTRUCTION RECORD North Carolina Department of Environment and Natural Resources Division of Water Quality WELL CONTRACTOR CERTIFICATION
- 3106 1. WELL CONTRACTOR:
James D. Barker Well Contractor (Individual)
Name Quantex, Inc.Well Contractor Company Name STREET ADDRESS P.O. Box 41673 Raleigh, NC 27629 City or Town State Zip Code (919 219-9604 Area code- Phone number 2. WELL INFORMATION:
SITEWELLIDiAiapplicable).
W "ZLL-L/ ,-'WELL CONSTRUCTION PERMIT#(11appicable)
NA OTHER ASSOCIATED PERMIT #(if applicable)
NA 3. WELL USE (Check Applicable Box) Monitoringl Municipal/Public13 Industiral/CommerciaC Agriculturall]
Recoveryt]
InjectionrI IrigatiorO OtherO (list use)DATE DRILLED 2/17/09 TIME COMPLETED 4! .30 AMR PME 4. WELL LOCATION: CITY: New Hill couNTY Wake New Hill Holleman Road, New Hill, NC 27562 (Street Name, Numbers. Community, Subdivision.
Lot No.. Parcel, Zip Code)TOPOGRAPHIC
/ LAND SETTING:# Slope 0 Valley 0 Flat 13 Ridge E Other.(check appropriate box) May be in degrees, LATITUDE N35 deg. 37.024' minutes, seconds or LONGITUDE W78 deg. 57.606' in a decimal formna Latitude/longitude source: I OPS 0 Topographic map (location of well must be shown on a USGS topo map and attached to this form if not using GPS)5. FACIULTY.
is me of the business whie the wau Is tocted.FACILITY ID #(if applicable)
NA NAME OF FACILITY Progress Energy Shearon H. Plant STREET ADDRESS New Hill Holleman Road New Hill NC 27562 d. TOP OF CASING IS 2.5' FT. Above Land Surface**Top of casing terminated atlor below land surface may require a variance in accordance with 15A NCAC 2C .0118.e. YIELD (gpm): NA METHOD OF TEST NA f. DISINFECTION:
Type NA Amount NA g. WATER ZONES (depth):.(Fromj To i" From To From _ To _ From_ To From To _ From To._7. CASING: ( Depth , f Diameter Thickness/Weight Material Fromn TOS Ft 2" sch40 PVC From To Ft.From_ ___To Ft.8. GROUT: (Depth Material Method From 0 To Ft. Neat Cement Pour From= To--'r- Ft Bentonite Place From _ To_ FL 9. SCREEN: I Depth " Diameter Slot Size Material From _.. To Ft 2" In. 0.010 In. PVC From To Ft. in.From_____
To Ft. In. In.10. SANDIGRAVEL PACK: Depth , Size Material From -ia Tol Ft. #2 Silica Sand From To___ __ Ft._From To_ Ft.11.DRILUNG LOG From To Formation Description
- 12. REMARKS: City or Town State Zip Code CONTACT PERSON Tim Silar MAILING ADDRESS New Hill Holleman Road New Hill NC 27562 City or Town State Zip Code)- NA Area code -Phone number 6. WELL DETAILS: a. TOTAL DEPTH: b. DOES WELL REPLACE EXISTING WELL? YESn NOW c. WATER LEVEL Below Top of Casing: NA FT (Use "+ if Above Top of Casing)1D0 NC CERLFy ..T m D L AS CONSTRCTED IN ACCORDANCE WITH iSA N9LACIC, WELLCýN RIUCi fT4DARDS, AND THAT A COPY OF THIS RECM 1166WEN I ELL OWNER.SIGNA*JRE OF CERTIFIED WELL CONTRACTOR James D. Barker DATE PRINTED NAME OF PERSON CONSTRUCTING THE WELL Submit the original to the Division of Water Quality within 30 days. Attn: Information Mgt., 1617 Mail Service Center- Raleigh, NC 27699-1617 Phone No. (919),733-7015 ext 568.Form GW-lb Rev.12/07 ss.tXt Cooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 Appendix C Field Notes 2 S'p.. ...... ..... ...... ...-- --- ------..... ... .----.....
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_Z 2 --......-~ ~ ~ ~ ---- -1.3 K v ' -----.. .. ....... ......../..... -.5 b ......~ .....a.q 27 U.U.-I a.em U.em-S a.-S SS.CýýCooling Tower Blowdown Line Assessment Report Shearon Harris Nuclear Power Plant April 2009 Appendix D Calculations APPENDIX D CALCULATIONS Groundwater Velocity Calculation V/s-K (dh/dl)V/s dh dl ne= Groundwater Velocity-Water Elevation Difference BDL-MW5 to BDL-MW8 = 4.99'= Horizontal Distance Difference BDL-MW6 to BDL-MW8 = 200'K = Hydraulic Conductivity 1.14 ft/day (Arithmetic Mean Value from Table 2.4.12-208, FSAR)ne = Porosity = 5%(Freeze and Cherry, 1979)V/s =1.14 ft/day V/s = 0.529 ft/day= 193 ft/year (4.99 ft/215 ft).05