ML20117M791

Standby Nuclear SW Pond Physical Testing Conducted During Feb 1995

ML20117M791
Person / Time
Site:	Catawba
Issue date:	02/28/1995
From:	Randy Baker DUKE POWER CO.
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ML20117M776	List: ML20117M773 ML20117M782 ML20117M791 ML20117M802
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NUDOCS 9609180098
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i I

5TPrCHMD J TL Catawba Standby Nuclear Service Water Pond Physical Testing Conducted During February 1995 1

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Richard E. Baker, Jr., P.E., Senior Engineer Environmental Engineering Duke Power Comp:ny 9609180098 960910 DR ADOCK0500g3

Catawba SNSWP Page1of7 R. E. Baker Catawba SNSWP Stratification Testing Testing was conducted at Catawba during the time period of February 12-14,1995. The purpose of the testing was to examine the stratification effects of a heated discharge into the SNSWP. The SNSWP is assumed to be a series of stratified layers in the computer simulation described in CNC-Il50.01-00-0001. This testing was possible because the SNSWP was aligned for cooling during this time period due to RN valve work.

'The objectives of this testing were to:

e Verify existence of stratification.

. Verify heated surface layer spreads out over the SNSWP.

• Verify heated layer is not withdrawn at intake.

• Verify the flow is not shon-circuiting between the short-arm dischart e and the intake.

Test Conditions

• The SNSWP was aligned for cooling flow at 0200 on 2/12 and realigned at -

approximately 1300 on 2/14.

. Flow during the test period was approximately 11,400 gpm (25.4 cfs) for the first 7 hours8.101852e-5 days <br />0.00194 hours <br />1.157407e-5 weeks <br />2.6635e-6 months <br /> and 10,700 gpm (23.8 cfs) for the remaining time period.

• The associated AT (difference between intake and discharge temperatures) was 15 - 20*F.

+ The heat load rejected to the SNSWP during this time period was approximately 40%

of that denf.hd in CNC-1150.01-00-0001.

• During the first day of testing (2/12), the prevailing wind direction was from the northeast (Lake Wylie towards the shon-arm discharge structure).

Testing Methods Temperature Surface temperature measurements were continuously collected (at I m depth) during the test period at the following locations (see Figure 1):

• Short Arm -1

. Short Arm - 2

• Long Arm - 1

• Intake

Cattwba SNSWP

' Page 2 of 7 R. E. Baker

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A temperature profile at the Intake (from a raft) was continuously collected at the following depths (and are labeled on the attached graphs as noted):

. ' I m (Raft-1)

• 3 m (Raft-3) 5 m (Raft-5)

. Bottom (approximately 8 m)(Bottom)

Additional (grab sample) temperature measurements (resulting in profiles) were taken at  ;

other locations (see Figure 1) as follows:  !

. D - Discharge structure in short-arm

. 3 - Point in short-arm between discharge and intake

. 7 - Point in long-arm

. 8 - Point in long-arm e I -Intake Dve Testina A slug addition of Rhodamine WT dye was made between 0945 and 1030 on 2/12 and the dye movement through the pond was analyzed using fluorometer measurements.

l

-A fluorometer was used at the intake (approximately 25 ft deep) to continuously sample pond effluent to determine the first presence of dye being returned to the plant.

Dye measurements (grab samples / depth profiles) were taken at the locations previously described (D, 3, 7, 8, I).

Transects were run at three different depths (0.3 m, I m, and 3 m ) across the short-arm to analyze the spread of the dye.

Photographs were taken to show the surface spread of the dye to record visual observations of the testing results.

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Cotawba SNSWP Page 3 of 7 R. E. Baker .

I Results Elow No flow was observed from the long-arm discharge structure which resulted in a conservative testing scenario with regard to the spreading of the heated discharge layer. A higher flowrate from the station would result in flow from the long-arm discharge which would aid in ensuring a complete surface spread of the heated water.

Temocrature Temperatures at the intake remained stratified for the duration of the testing period as ,

shown in Figures 2 and 3. The surface temperature increased from an initial temperature l of 42 - 43*F (prior to alignment of the SNSWP for cooling) to a temperature of up to I 48'F (Figure 2). The temperature at I m depth (see Figure 3) remained greater than 46'F while the temperature at the depth of the intake (8 meters) remained below 43*F.

Figure 4 shows the similarity of the continuous surface temperature measurements (collected at I m depths) located at: i e Short arm - 1

• Short arm - 2

• Raft -1

• Long Arm -1 l l

Before the start of the testing period (2/11 @l900 - 2/12 @0200), the four probes had similar temperatures of 43 - 44*F. After discharge (and recirculation) of the SNSWP began at 0200, the first probe in the short-arm (Short Arm-1) measured an increasing temperature. In a series, the other probes (Short Arm-2, Raft-1,' and Long Arm-1) measured increasing temperatures. These temperature increases demonstrate the surface spread of the heated layer.

Figure 5 shows the stratification of the water column at Location 3 (see Figure 1). The surface temperature increased approximately 9'F while the temperature at the bottom remained unchanged. The surface temperature remained elevated during the testing period while the bottom layer temperature remained unchanged from initial conditions.

Figure 6 shows the temperature stratification at the discharge structure in the short-arm of the SNSWP. The data shows that the heated discharge remains in the upper 2 ft of the water column as it enters the SNSWP. Again, the water column at this point remained stratified for the duration of the test.

Figure 7 shows a combination of the grab sample results at locations 7 and 8 (see Figure 1). These two sets of results were combined because of the close proximity of the

- locations. The observed stratification at these locations further demonstrates the complete surface spread of the heated layer and the associated stratified layers.

h I

Catawba SNSWP Page 4 of 7  ;

R. E. Baker l Dve Testina l Figure 8 shows the observed dye concentrations at the intake during the test period. The I l

surface dye concentrations increased from 12 ppb on 2/12 to 48 ppb on 2/13. After this observed maximum concentration,' the dye concentrations showed movement down l through the water column as a layer (see 2/13 @l324 data). This downward moving layer l was also observed during the last sampling period (2/14 @l211). These measurements  :

demonstrate the surface spread of the heated layer to the intake and stratification of the water column.

' Figures 9 and 10 show the stratifed layers at location 3 (see Figure 1). Again, after the maximum dye concentration was observed, the dye moved down through the water column as a stratified layer.

Figure 11 shows the observed dye concentrations at locations 7 and 8. The location 7 data (2/12) demonstrates the surface spread of the heated discharge layer into the long-arm and the associated stratification while the location 8 data (2/13) shows the movement of the stratified layer down through the water column.

Dye concentrations collected at various depths along Transect 1 (see location on Figure 1) in the short-arm (see Figures 12,13 and 14) show that dye covered the entire width of the  !

short-arm. Note, the data shown in Figure 12 exceeded the instrument range of 1000 ppb.  !

i The comparison of dye concentrations Figure 13 (3 ft depth) and Figure 14 (6 ft depth) demonstrates the stratification of the water column.

Additionally, the complete dye spread over the entire SNSWP surface is presented in the l

attached photographs. (See attachments)

Catawba SNSWP l Page 5 of 7 R. E. Baker Evaluation of Results Observed Results durina Physical Testine The similarity'of the surface temperatures (Figure 4) in comparison to the differences of -

the intake temperatures (Figure 3) demonstrate the existence of a stratified flow pattern instead of a plug-flow pattern. q The continued stratification at the intake and the complete surface spread demonstrates that there is not a short-circuiting eff-t:t caused by the short distance between the short-arm discharge and intake in comparison to the distance between the long-arm discharge  ;

and intake. The stratification allowed for surface cooling of the heated discharge layer l prior to its shifting down and replacement by additional heated discharge flow. Thus, the heated lay;r was prevented from being withdrawn at the intake.

l Heated Laver Thickness ,

Information from the dye testing and temperature monitoring can be used to determine the depth of the heated layer. The dye spread completely over the SNSWP surface in less  ;

than 24 hours2.777778e-4 days <br />0.00667 hours <br />3.968254e-5 weeks <br />9.132e-6 months <br />. The flowrates during the test period were lower than the values described j in CNC-1150.01-00-0001. The flowrate for the first 7 hours8.101852e-5 days <br />0.00194 hours <br />1.157407e-5 weeks <br />2.6635e-6 months <br /> was 25.4 cfs and 23.8 cfs for j the remaining time period. These flowrates can be used to determine the total volume of heated water discharge to the SNSWP in a given time period. Since the dye addition  :

began at 0945 and ended at 1030, the 23.8 cfs value can be used to determine the total volume discharged at the time the leading edge was observed to reach certain points (see table below). These values can be used to determine a depth of the heated layer. ,

l Heated Layer Thickness Based on Dye Testing Location TomeDye Reached Total Volume Area no kcation Depth ofHeated Locasson after Start Dischargedto (sf) Layer ft) .

of(0945) Dye ShlSWP(cf)

Addition (hours)

Short Arm-2 3 257,040 335,663 0.8 Intake 4 342,720 461,738 0.8 Entire - <22 1,884,960 1,529,392 1.2 Surface Note, the time for the dye to cover the entire surface was actually less than 22 hours2.546296e-4 days <br />0.00611 hours <br />3.637566e-5 weeks <br />8.371e-6 months <br />, but the exact time cannot be established.

e

l 1

a Catawba SNSWP Page 6 of 7 l R. E. Baker  !

i (-

A similar approach can be used to determine the heated layer depths based on the time for the temperature to start rising at different locations.

l Heated Layer Thickness Based on Temperature l Location Dme of Forst Total Volume Area to Locotton Depth ofHeased Temperature at Deschargedto (Af) Layer @)

locatnonDp SNSWP(cf) I anachedLocation l i +rstaru #2x) l DyAddition thours)

Short Arm-2 4.5 411,480 335,663 1.2 Intake 5.5 502,920 461,738 1.1 Long Arm-1 12 1,068,480 963,429 1.1 From these two methods, the heated layer thickness is less than 2 ft which is in close agreement with assumptions used in CNC-1150.01-00-0001.

Tvoe of Flow Model The SNSWP cooling effectiveness can be . evaluated using average February meteorological conditions, reduced heat loads to account for only one unit being cooled during the Febmary testing period, and an initial SNSWP temperature of 42*F in the SNSWP model (stratified flow) described in CNC-Il50.01-00-0001 and comparing the output with results from a plug-flow model. The following table summarizes the results of the two flow types modeled and the physical testing results.

FlowModel Comparison. ,

I

. Posnt Destancefrom PredsetedPlug. Obsernd SNSWPModel Obsernd S4 Discharge FlowModel Maxsmum (Stratiped) Man' mum

@) Temperature Temperature Temperature aper Temperatures During Physucal Surface Coohng at Testing (1 m depth 19 depth (aper from Forure 31 22 hours2.546296e-4 days <br />0.00611 hours <br />3.637566e-5 weeks <br />8.371e-6 months <br /> >

SA Discharge 0 62 62 (Fig. 6) 51 59 SA-1 480 59.7 52 51 50 SA-2 850 58.2 51.5 51 -

Intake 1111 57.7 49.5 51 50 LA-1 1800 54.9 47.5 51 45 Observations from the two models The plug-flow model temperatures are always greater than the observed values during the physical testing while the stratified-flow results are similar to the observed values for both the maximum observed temperature values and ,the 1 ft depth maximums after 22 hours2.546296e-4 days <br />0.00611 hours <br />3.637566e-5 weeks <br />8.371e-6 months <br />.

From this comparison of model output, the stratified model is providing reasonable results. l J

Catawba SNSWP Page 7 of 7 R. E. Baker r

Conclusions Stratification exists in the SNSWP even with low AT conditions tested.

l There is no short-circuiting of flow between the discharge and intake on the short-arm. '

The heated discharge spreads completely over the SNSWP to achieve maximum surface i

cooling, and the SNSWP remained stratified dudng the testing period. j The heated surface layer is approximately 1 ft thick, and this value is in agreement with -

CNC-1150.01-00-0001. l i

The existing assumptions in the Catawba SNSWP model (reference CNC-1150.01 0001) are valid and no corrections to the model are necessary. l i

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4 0

Catawba SNSWP l

R. E. Baker

]

List of Attachments I

(

i Figures ,

l Data Tables Photographs

' Stratified Flow Model Results ,

Plug Flow Model Results i l

l l

l 1

l l

i I

Catawba SNSWP R. E. Baker 1

List of Figures Figure 1 Test Locations Figure 2 CNS SNSWP - Location I - Variation of Temperature with Depth Figure 3 Catawba Nuclear Station - SNSWP - Variation of Temperature with Depth at Intake Figure 4 Catawba Nuclear Station - SNSWP - Variation of Surface Tempercture with Distance from Short-Arm Discharge Figure 5 CNS SNSWP - Location 3 - Variation of Temperature with Depth Figure 6 CNS SNSWP - Location D - Variation of Temperature ivith Depth Figure 7 CNS SNSWP - Locations 7 & 8 - Variation of Temperature with Depth ,

Figure 8 CNS SNSWP - Location I - Variation of Dye Concentration with Depth - 1 Figure 9 CNS SNSWP - Location 3 (Abbreviated Dye Concentration Scale) -

Variation of Dye Concentration with Depth Figure 10 CNS SNSWP - Location 3 - Variation of Dye Concentration with Depth Figure 11 CNS SNSWP - Locations 7 and 8 - Variation of Dye Concentration with j 1

Depth Figure 12 Transect 1 (One-foot) February 12,1995 Figure 13 Transect 1 (Three-foot) February 12,1995 Figure 14 Transect 1 (Six-foot) February 12,1995 I

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l LOC DATE TIME TEMP DEPTH

- (no) (dd-m-yy) (hhmmss) (deg-F) (ft)

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1 12-Feb-95 4541 43.3 1 l

1 12-Feb-95 4621 43.1 3.3 1 12-Feb-95 4656 43.1 6.6

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1 12-Feb-95 4751' 43.1 9.8 I 12-Feb-95 4836 42.5 13.1 1 12-Feb-95 4921 42.2 16.4 i

i 12-Feb-95 5001 42.1 19.7 1 12-Feb-95 5046 41.9 23 1 12-Feb-95 5121 41.9 25.3 1 1 12-Feb-95 52112 42.8 1 1 12-Feb-95 52137 42.8 2 1 12-Feb-95 52157 42.8 3  ;

i 12-Feb-95 52217 42.8 4 j l 12-Feb-95 52232 42.8 5 1 12-Feb-95 52252 42.8 6 1 12-Feb-95 52317 42.8 7 1 12-Feb-95 52337 42.8 8 j l 12-Feb-95 52357 42.8 9 l 12-Feb-95 52417 42.8 10 1 12-Feb-95 52442 42.8 11 1 12-Feb-95 52502 42.7 12 1 12-Feb-95 52522 42.7 13 1 12-Feb-95 52537 42.7 14 1 12-Feb-95 52557 42.5 15 1 12-Feb-95 52612 42.4 16 1 12-Feb-95 52627 42.3 17 l 12-Feb-95 52647 42.1 18 l 12-Feb-95 52707 42.1 19 1 12-Feb-95 52722 42.1 20 1 12-Feb-95 52742 42.1 21 1 12-Feb-95 52802 42 21.9 l 12-Feb-95 52817 42 23 1 12-Feb-95 52837 42 24 1 12-Feb-95 52852 41.9 25 1 12-Feb-95 134018 45.2 1 1 12-Feb-95 134053 44.6 2 1 12-Feb-95 134113 44.5 3

-1 12-Feb-95 134133 43.8 4 1 12-Feb-95 134153 43.7 5 1 12-Feb-95 134218 43.6 6 1 12-Feb-95 134233 43.6 7 1 12-Feb-95 134258 43.5 8

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I 12-Feb-95 134318 43.4 9 l 12-Feb-95 134333 43.3 10 '

1 12-Feb-95 134348 43.3 11 i 12-Feb-95 134408 43.2 12 I i 12-Feb-95 134428 43.2 13 1 12-Feb-95 134448 43.2 14 i 12-Feb-95 134508 43.2 15 1 12-Feb-95 134523 43.1 16

i 12-Feb-95 134538 43.1 17 l 12-Feb-95 134553 43.1 18 l 12-Feb-95 134608 43 19 l 12-Feb-95 134633 42.9 20 1 12-Feb-95 134648 42.9 21 1 12-Feb-95 134708 42.7 22 1 12-Feb-95 134728 42.6 23 1 12-Feb-95 134748 42.5 24 1 12-Feb-95 134808 42.5 25 11 12-Feb-95 165604 49.8 1 11 12-Feb-95 165629 48.6 2 11 12-Feb-95 165704 46.6 3 11 12-Feb-95 165729 45.4 4 11 12-Feb-95 165749 44.1 5 4

11 12-Feb-95 165809 43.7 6 I

11 12-Feb-95 165829 43.6 7 11 12-Feb-95 165854 43.6 8  !

43.6 9 l 11 12-Feb-95 165914

• 11 12-Feb-95 165934 43.4 10 11 12-Feb-95 165949 43.3 11 11 12-Feb-95 170004 43.2 12 11 12-Feb-95 170024 43.3 13 4 11 12-Feb-95 170044 42.8 14 11 12-Feb-95 170104 42.6 15 l 11 12-Feb-95 170124 42.5 16 11 12-Feb-95 170144 42.4 17

! 11 12-Feb-95 170159 42.4 18 11 12-Feb-95 170219 42.4 19 11 12-Feb-95 170234 42.3 20 11 12-Feb-95 170254 42.4 21 I 11 12-Feb-95 170309 42.5 22 11 12-Feb-95 170329 42.5 23 11 12-Feb-95 170354 42.4 24 i 11 12-Feb-95 170414 42.4 25 11 12-Feb-95 170434 42.2 26 11 12-Feb-95 170454 42.2 27 11 12-Feb-95 170509 42.2 28 a

I LOC DATE TIME TEMP DEPTH (no) (dd-m-yy) (hhmmss) (deg-F) (ft) f 11 12-Feb-95 170529 42.2 29 11 12-Feb-95 170544 42.2 30 L

i 13-Feb-95 131829 49.7 1 1 13-Feb-95 131844 47.9 2 1 13-Feb.95 131914. 47 5 3 1 13-Feb-95 131934 46 4 1 13-Feb-95 131949 45.6 5 1 13-Feb-95 132009- 44.5 6 l 13-Fet> 95 132034 44.1 7 1 13-Feb-95 132059 44 8 I 13-Feb-95 132119 43.8 9 -

f I 13-Feb-95 132139 43.6 10 i 13-Feb-95 ,132159 43.5 11 l~ l 13-Feb-95 132219 43.3 12 1 13-Feb-95 132234 43.3 13 1 13-Feb-95 132259 43.1 14'

1 13-Feb-95 132324 43.1 15

! I 13-Feb-95 132344 43.1 16 l l 13-Feb-95 132404 43.1 17 l 13-Feb.95 132419 43.1 18

1 13-Feb-95 132434 43.1 19 l 13-Feb-95 .132509 43 20 1 13-Feb-95 132529 43 21 1 13-Feb-95 132549 42.9 22

!- l 13-Feb-95 132609 42.8 23 1 13-Feb-95 132624 42.8 24 1 13-Feb-95 132644 42.7 25 l 13-Feb-95 132659 42.7 25.8 l

11 13-Feb-95 93748 46.3 1 11 13-Feb-95 93813 46.3 2 i 11 13-Feb-95 93828 46.2 3

.11 13-Feb-95 93848- 45.6 4 11 13-Feb-95 93908 45.6 5

. 11 13-Feb-95 93928 45.5 6 l

li ' 13-Feb-95 93943 44.1 .7 11 13-Feb-95 93958' 43.8 8

'11 13-Feb-95 94023- 43.7 9 It ' 13-Feb-95 : 94043 43.7 10 11 13-Feb-95 94058 43.7 11 11 13-Feb-95 94113 43.3 12 ,

13-Feb-95 94133 43.3 13

!. 11

! 11 13-Feb-95 94158 43.3 14

[ 11 13-Feb-95 94218 43.2 15 i 11 13-Feb-95 94233 43.2 16 i

~ '

I _ . . ~ . -., , . - , .

LOC DATE TIME TEMP DEPTH

[- (no) (dd-m-yy) (hhmmss) (deg-F) (ft) 13-Feb-95 94253 43.2 17 11 11 13-Feb-95 94313 43.1 18 11 13-Feb-95 94328' 43.1 19 11 13-Feb-95 94343 43 20 11 13-Feb-95 94358 42.9 21 l 11 13-Feb-95 94413 42.9 22 11 13-Feb-95 94428 42.8 23 11 13-Feb-95 94448 42.7 24 11 13-Feb-95 94508 42.7 25 11 13-Feb-95 94528 42.7 26 11 13-Feb-95 94543 42.6 27 11 13-Feb-95 94603 42.5 28 11 13-Feb-95 94618 42.5 29 11 13-Feb-95 94628 42.5 29.4 1 14-Feb-95 120218 48.2 1 1 14-Feb-95 120248 48.1 2 1 14-Feb-95 120328 47.1 3 1 14-Feb-95 120348 46.9 4 l 14-Feb-95 120428 46.8 5 1 14-Feb-95 120448 46.3 6 1 14-Feb-95 120513 46 7 1 14-Feb-95 120603 45.9 8 1 14-Feb-95 120633 45.9 9 l 14-Feb-95 120703 45.7 10 1 14-Feb-95 120733 45.6 11 1 14-Feb-95 120753 45.4 12

-l 14-Feb-95 120813 45 13 1 14-Feb-95 120843 44.7 14  !

I 14-Feb-95 120918 44.1 15 i i 14-Feb-95 120943 43.9 16 1 14-Feb-95 121008 43.8 17 1 14-Feb-95 121043 43.7 18 l 14-Feb-95 121128 43.3 19 l 14-Feb-95 121158 43.1 20 1 14-Feb-95 121223 43.1 21 l l 14-Feb-95 121308 43.1 22 l 14-Feb-95 121328 43.1- 23 1 14-Feb-95 121353 43 24 1 14-Feb-95 121413 43 25 l 14-Feb-95 121443 43 25.3 j 4

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LOC DATE TIME TEMP DEPTH (no) (dd-m-yy) (hhmmss) (deg-F) - (ft) ,

1

! D 14-Feb-95 113713 62.4 1 D 14-Feb-95 113828 54.1 2-D 14-Feb-95 113943 52.6 3 i D 14-Feb-95 114058 47.6 4 4.6 D 14-Feb-95 114148 47.7  ;

. i D 13-Feb-95 133554 58.9 - 1 D 13-Feb-95 133614 54.8 2 .

D 13-Feb-95 133639 55.7 3 I D 13-Feb-95 133659 53 4 1

D 13-Feb-95 133734 51.8 5 D 13-Feb-95 133804 51.8 5.2 a D 12 Feb-95 44047 65.4 1 D 12-Feb-95 44117 50.9 2 D 12-Feb-95 44137 51.1 3 i D 12-Feb-95 44152 43.2 4

! D 12-Feb-95 44212 43.2 4.6 D 12-Feb-95 55107 59.9 1 D 12-Feb-95 55132 53.1 2 D 12-Feb-95 55207 49.9 3 D 12-Feb-95 55227 44.9 4 D 12-Feb-95 55247 43.8 4.6 4

I l

l LOC DATE TIME TEMP DEPTH J (no) (dd-m-yy) (hhmmss) (deg-F) (ft) j 3 12-Feb-95 50032 45.8 1 3 12-Feb-95 50047 45.5 2 3 12-Feb-95 50112 44.6 3 l 3 12-Feb-95 50132 43.4 4 3 12-Feb-95 50152 43.2 5 3 12-Feb-95 50207 43.3 6 3 12-Feb-95 50227 43.3 7 3 12-Feb-95 50252 43.3 8 3 12-Feb-95 '50312 43.5 9 1 3 12-Feb-95 50327- 43.6 10 l 3 12-Feb-95 50342 43.6 11 3 12-Feb-95 50402 43.4 12 i

3 12-Feb-95 95359 49.8 1 l 3 12-Feb-95 95429 49.8 2 3 12-Feb-95 95539 45.5 3 1 3 12-Feb-95 95909 48.4 4 3 12-Feb-95 95944 48.1 5 3 12-Feb-95 100009 47.1 6 3 12-Feb-95 100024 46.6 7 3 12 Feb-95 100044 43.4 8 3 12-Feb-95 100109 42.9 9 3 12-Feb-95 100124 42.9 10 3 12-Feb-95 100149 42.8 11 3 12-Feb-95 100204 42.7 12 3 12-Feb-95 ' 100229 42.7 13 3 12-Feb-95 100244 42.7 14 3 12-Feb-95 100259 42.7 14.7 1 .

+

LOC DATE TIME TEMP DEPTH (dd-m-yy) (hhmmss) (deg-F) (ft) f (no) 3 12-Feb-95 144239 53.4 1 3 12-Feb-95 144259 53.3 2 ,

3 12-Feb-95 144314 53.4 3 3 12-Feb-95 144409 50.4 4 3 12-Feb-95 144449 45.6 5 3 12-Feb-95 144509 45.2 6 3 12-Feb-95 144534 44.7 7 3 12-Feb-95 144604 44.9 8 l

3 12-Feb-95 144629 44.5 9 ~

3 12-Feb-95 144649 43.7 10 3 12-Feb-95 144709 43.5 11 3 12-Feb-95 144729 43.1 12 3 12-Feb-95 144749 43.1 13 .

3 12-Feb-95 144809 43.1 14 3 12-Feb-95 144824 43 14.8 I

I I

. 3 12-Feb-95 164444 52.2 1

. 3 12-Feb-95 164459 52.2 2 i I

i 3 12-Feb-95 164519 51.9 3 3 12-Feb-95 164539 52.2 4 3 12-Feb-95 164554 51.6 5 3 12-Feb-95 164619 46.8 6 l 3 12-Feb-95 164639 43.7 7 3

3 12-Feb-95 164659 43.8 8 3 12-Feb-95 164714 43.7 9 3 12-Feb-95 164729 43.3 10  ;

< 3 12-Feb-95 164749 43.2 11 j 3 12-Feb-95 164804 43.2 12 3 12-Feb-95 164819 43.1 13 1 a 3 12-Feb-95 164834 43.1 14 3 12-Feb 95 164854 43.1 15 1 j 3 12-Feb-95 '164909 43.1 15.7 d

3 13-Feb-95 100818 50.3 1 3 13-Feb-95 100833 50.2 2 3 13-Feb-95 100848 50.2 3 J

3 13-Feb-95 100903 50 4 3 13-Feb-95 100923 49.6 5 3 13-Feb-95 100948 49.4 6 3 13-Feb-95 101008 48.3 7

, 3 13-Feb-95 101028 48.3 8 3 13-Feb-95 101043 48.3 9 3 13-Feb-95 101058 47.9 10 .

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LOC DATE TIME TEMP DEPTH i (no) (dd-m-yy) (hhmmss) (deg-F) (ft) - (

3 13-Feb-95 101213 44.4 11 i 3 13-Feb-95 101238 43.5 12 3 13-Feb 101258 43.4 13 3 13-Feb-95 101313 43.3 14 3' 13-Feb-95 101338 43.2 15 3 13-Feb-95 101353 43.2 15.6 .

1

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-3 13-Feb-95 125219 50.5 1 3 13-Feb-95 125239 49.9 2 3 13-Feb-95 125304 49.7 3 3 13-Feb-95 125319 49.4 4 3 13-Feb-95 125339 49.8 5 3 13-Feb-95 .125359 48.9 6 3 13-Feb-95 125414 48 7 3 13-Feb-95 125429 47 8 3 13-Feb-95 125444 44 9 3 13-Feb-95 125504 43.6 10 l

l 3 13-Feb-95 125524 43.4 11 3 13-Feb-95 125539 43.4 12 3 13-Feb-95 125554 43.3 '13 3 13-Feb 95 125614 43.3 14 3 13-Feb-95 125C29 43.2 15 3 13-Feb-95 125644 43.1 16 i

.3 14-Feb-95 114638 48 1 3 14-Feb-95 114728 47.8 2 )

1 3 14-Feb-95 114758 47.7 3 3 14-Feb-95 114823 47.5 4 l 3 14-Feb-95 114908 47.1 5 3 14-Feb-95 114933 46.6 6 l

3 14-Feb-95 115008 45.5 7 3 14-Feb-95 115103 45.3 8 l

3 14-Feb-95 115133 45.1 9 3 ' 14-Feb-95 115208 44.7 10 3 14-Feb-95 115238 44.5 11  ;

l 3 14-Feb-95 115318 44.3 12 ]

3 14-Feb-95 115343 44 13 3 14-Feb-95 115413 43.9 14 3 14-Feb-95 115433 43.8 15 3 14-Feb-95 115453 43.8 15.4

LOC DATE TIME TEMP DEPTH (no) (dd-m-yy) (hhmmss) (de9-F) (ft) 8 13-Feb-95 102258 44.9 1 8 13-Feb-95 102313 44.9 2 8 13-Feb-95 102338 44.9 3 l 8 13-Feb-95 102358 44.9 4 8 13-Feb-95 102418 44.9 5 8 13-Feb-95 102433 44.9 6 8 13-Feb-95 102458 44.9 7 l i

8 13-Feb-95 102513 44.9 8 8 13-Feb-95 102528 44.8 9  !

l 8 13-Feb-95 102538 44.8 10 l

8 13-Feb-95 102553 44.6 11 0 13-Feb-95 102608 44.5 12 8 13-Feb-95 102628 44.5 13 8 13-Feb-95 102638 44.1 14 8 13-Feb-95 102653 43.1 15 l 8 13-Feb-95 102708 43 16 i

8 13-Feb-95 102723 42.9 17 I

8 13-Feb-95 102733 42.9 18 8 13-Feb-95 130519 45 1 8 13-Feb 130534 45 2 8 13-Feb-95 130604 44.9 3 8 13-Feb 95 130624 44.8 4 8 13-Feb-95 130639 44.7 5 8 13-Feb-95 130704 44.6 6 8 13-Feb-95 130724 44.6 7 8 13-Feb-95 130744 44.6 8 8 13-Feb-95 130809 44.6 9 8 13-Feb-95 130829 44.6 10 8 13-Feb-95 130849 44.4 11 8 13-Feb-95 130919 44.2 12 8 13-Feb-95 130949 44.1 13 8 13-Feb-95 131009 43.9 14 8 13-Feb-95 131024 43.7 15  ;

8 13-Feb-95 131044 43.6 16 8 13-Feb-95 131104 43.2 17 8 13-Feb-95 131124 42.9 18 8 13-Feb-95 131139 42.9 18.4  ;

I i

1 LOC DATE TIME TEMP DEPTH l (no) - (dd-m-yy) (hhmmss) (deg-F) (ft)

[

8 14-Feb-95 123443 46.5 1 8 14 Feb-95 123523 46.3 2 l 123628 46.2 3 l 8 14-Feb-95 8 14-Feb-95 123653 46.1 4 8 14-Feb-95 123718 46.1 5 8 14-Feb-95 123733 45.9 6 8 14-Feb-95 123808 45.9 7 P 14-Feb-95 123833 45.9 8 8 14-Feb-95 123853 45.7 9 j 8 14-Feb-95 123918 45.6 10 j 8 14-Feb-95 123953 45.1 11 8 14-Feb-95 124018 45 12 8 14-Feb-95 124053 44.7 13 8 14-Feb.95 124123 44.6 14 8 14-Feb-95 124143 44.1 15 8 14-Feb-95 124213 44 16 ,

8 14-Feb-95 124238 43.8 17 8 14-Feb-95 124258 43.6 17.4 1 7 12-Feb-95 163034 45.9 1 7 12-Feb-95 163059 45.4 2 1 7 12-Feb-95 163124 44.1 3 7 12-Feb-95 163144 43.7 4 7 12-Feb-95 163204 43.6 5 7 12-Feb-95 163224 43.6 6 7 12-Feb-95 163244 43.6 7 7 12-Feb-95 163259 43.5 8 7 12-Feb-95 163319 43.4 9 7 12-Feb-95 163339 43.3 10 7 12-Feb-95 163354 43.3 11 7 12-Feb-95 163409 43.2 12 7 12-Feb-95 163429 42.9 13 7 12-Feb-95 163449 42.8 14

15 7 12-Feb 163509 42.7 7 12-Feb 163529 42.4 16 7 12-Feb-95 163549 42.4 17 7 12-Feb-95 163614 42.3 18 7 12-Feb-95 163634 42.2 19

' 19.8 7 12-Feb-95 163649 42.1 i

0 4

4

Date Loc Time Dye Conc Depth Dye Conc Depth g( fddmmyy) (hhmm) (ppb) (meters) (ppb) - ft 12-Feb-95 1 52 0.09 0.3 0.09 -0.98424 12-Feb-95 1 53 0.04 1 0.04 3.2808 12-Feb-95 1 54 0.03 2 0.03 6.5616 12-Feb-95 I 55 0.05 3 0.05 9.8424 12-Feb-95 I 56 0.05 4 0.05 13.1232 12-Feb-95 I 57 0.05 5 0.05 16.404 i 12-Feb-95 1 58 0.04 6 0.04 19.6848 j 12-Feb-95 I 59 0.03 7 0.03 22.9656 12-Feb-95 1 100 0.06 7.7 0.06 25.26216 )

1 12-Feb-95 l 1344 11.78 0.3 11.78 0.98424 i 12-Feb-95 1 1345 8.44 1 8.44 3.2808 i 12-Feb-95 1 1346 6.61 2 6.61 6.5616 12-Feb-95 1 1347 1.2 3 1.2 9.8424 12-Feb-95 1 1348 0.05 4 0.05 13.1232 12-Feb-95 l 1349 0.05 5 0.05 16.404 j 12-Feb-95 1 1350 0.04 6 0.04 . -19,6848 l 12-Feb-95 i 1351 0.1 7 0.1 '22.9656 I 12-Feb-95. I 1352 0.03 8 0.03 26.2464 12-Feb-95 1 1353 0.02 9 0.02 29.5272 13-Feb-95 1 1047 48.4 0.3 48.4 0.98424 13-Feb-95 1 1048 45.66 - 1 45.66 3.2808 13-Feb-95 1 1049 39.43 2 39.43 6.5616 13-Feb-95 1 1050 18.68 3 18.68 9.8424 13-Feb-95 1 1051 4.79 4 4.79 13.1232 j 13-Feb-95 1 1052 0.49 5 0.49 16.404 I 13-Feb-95 1 1053 0.13 6 0.13 19.6848 13-Feb-95 1 1054 0.04 7 0.04 22.9656 13-Feb-95 1 1055 0.04 8 0.04 26.2464 I

13-Feb-95 i 1323 15.55 0.3 15.55 0.98424 13-Feb-95 i 1324 45.82 1 45.82 3.2808 13-Feb-95 l 1325 19.25 2 19.25 6.5616 13-Feb-95 1 1326 16.45 3 16.45 9.8424 13-Feb-95 1 1327 4.66 4 4.66 13.1232 13-Feb-95 l 1328 1.68 5 1.68 16.404 :

13-Feb-95 l 1329 1.83 6 1.83 19.6848 13-Feb-95 1 1330 0.12 7 0.12 22.9656 l 13-Feb-95 -1 1331 0.07 8 0.07 26.2464 I

i Date Loc Time Dye Conc Depth Dye Conc Depth (ddmmyy) (hhmm) (ppb) (meters) (ppb) ft

(

14-Feb-95 1 1207 28.83 0.3 28.83 0.98424 l 14-Feb-95 1 1208 23.74 1 23.74 3.2808 14-Feb-95 l 1209 31.25 2 31.25 6.5616

-, 14-Feb-95 1 1210 39.01 3 39.01 9.8424 14-Feb-95 1 1211 69.62 4 69.62 13.1232

] 52.74 5 52.74 16.404 14-Feb-95 1 1212

', 14-Feb-95 1 1213 14.94 6 14.94 19.6848 14 Feb-95 1 1214 5.86 7 5.86 22.9656 14-Feb-95 1 1215 1.85 8 1.85 26.2464 -

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DATE LOC TIME DYE CONC DEPTH (ddmmyy) (hhmm) (ppb) (feet) (meters)

{ 2/12/95 1002 12-Feb-95 3 1002 0.08 0.98424 0.3 12-Feb-95 3 1003 0.05 3.2808 1 12-Feb-95 3 1004 0.03 6.5616 2 12-Feb-95 3 1005 0.02 9.8424 3 ,

12-Feb-95 3 1006 0.07 13.1232 4 2/12/95 1036 12-Feb-95 3 1036 1988.63 0.98424 0.3 12-Feb-95 3 1037 1568.07 3.2808 1 l 12-Feb-95 3 1038 1735.18 6.5616 2 l 12-Feb-95 3 1039 59.12 9.8424 3 I 12-Feb-95 3 1040 0.49 13.1232 4  !

2/12/95 /12/95 1446 l 12-Feb-95 3 1446 170.71 0.98424 0.3 12-Feb-95 3 1447 183.68 3.2808 1 12-Feb-95 3 1448 8.43 6.5616 2 12-Feb-95 3 1449 0.24 9.8424 3 12-Feb-95 3 1450 0.12 13.1232 4 12-Feb-95 3 1451 0.1 16.404 5 12-Feb-95 3 1452 0.32 19.6848 6 2/12/95 1648 12-Feb-95 3 1648 171.61 0.98424 0.3 12-Feb-95 3 1649 184.57 3.2808 1 12-Feb-95 3 1650 28.07 6.5616 2 12-Feb-95 3 1651 0.16 9.8424 3 12-Feb-95 3 1652 0.04 13.1232 4 12-Feb-95 3 1653 0.08 16.404 5 2/13/95 1012 13-Feb-95 3 1012 10.74 0.98424 0.3 13-Feb-95 3 1013 9.15 3.2808 1 13-Feb-95 3 1014 15.68 6.5616 2 ]

13-Feb-95 3 1015 10.6 9.8424 3 13-Feb-95 3 1016 0.82 13.1232 4 13-Feb-95 3 1017 0.21 16.404 5 2/13/95 1255 I 13-Feb-95 3 1255 10.07 0.98424 0.3 13-Feb-95 3 1256 15.02 3.2808 1 13-Feb-95 3 1257 33.65 6.5616 2 13-Feb-95 3 1258 1.13 9.8424 3 13-Feb-95 3 1259 0.74 13.1232 4 13-Feb-95 3 1300 0.14 16.404 5 2/14/95 1151 14-Feb-95 3 1151 32.88 0.98424 0.3 14-Feb-95 3 1152 36.48 3.2808 1 14-Feb-95 3 1153 40.55 6.5616 2 14-Feb-95 3 1154 65.05 9.8424 3 14-Feb-95 3 1155 56.6 13.1232 4 14-Feb-95 3 1156 23.88 16.404 5

Date Loc Time Dye Conc Depth Depth (ddmmyy) (hhmm) (ppb) - (feet) (meters) f 12-Feb-95 7 1634 26.63 0.98424 0.3 12-Feb-95 7 1635 2.3 3.2808 1 12-Feb-95 7 1636 0.91 6.5616 2 12-Feb-95 7 1637 0.22 9.8424 3 l 12-Feb-95 7 1638 0.03 13.1232 4 12-Feb-95 7 1639 0.04 .16.404 5 l i

12-Fet>95 7 1640 0.04 19.6848 6 1

13-Feb-95 8 1026 46.55 0.98424 0.3

' 13-Feb-95 8 1027 46.62 3.2808 1 13-Feb-95 8 1028 47.54 6.5616 2 13-Feb-95 8 1029 49.9 9.8424 3

i. 13-Feb 8 1030 55.67 13.123i 4 i 8 1031 12.09 16.404 5 l 13-Feb-95 13-Feb-95 8 1032 3.11 18.0444 5.5 l J

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Catawba SNSWP R. E. Baker Photographs and Descriptions

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Number Description i 1 2/12/95 9:40 am (Taken just before dye addition) Short-arm discharge  !

structure j 2 2/12/9510:00 am (15 min after start of dye injection) Taken from short-arm discharge structure 3 2/12/9510:00 am (15 min aner start of dye injection) Taken from bank opposite short-arm discharge structure ,

4 2/12/9510:30 am (45 min aRer start of dye injection) Taken from pier l looking up short-arm 5 2/12/9512:45 am (3 hour3.472222e-5 days <br />8.333333e-4 hours <br />4.960317e-6 weeks <br />1.1415e-6 months <br /> after start of dye injection) Taken from dam looking up short-arm 6 2/12/9512:45 am (3 hour3.472222e-5 days <br />8.333333e-4 hours <br />4.960317e-6 weeks <br />1.1415e-6 months <br /> after start of dye injection) Taken from pump-house hilllooking up short-arm l 7 2/12/9512:45 am (3 hour3.472222e-5 days <br />8.333333e-4 hours <br />4.960317e-6 weeks <br />1.1415e-6 months <br /> aner start of dye injection) Taken from pier stairway looking up short-arm 8 2/12/9512:45 am (3 hour3.472222e-5 days <br />8.333333e-4 hours <br />4.960317e-6 weeks <br />1.1415e-6 months <br /> after start of dye injection) Taken from pump-house hilllooking up short-arm  ;

9 2/12/9512:45 am (3 hour3.472222e-5 days <br />8.333333e-4 hours <br />4.960317e-6 weeks <br />1.1415e-6 months <br /> after start of dye injection) Taken from pump-3 house hilllooking up short-arm 10 2/12/951:45 pm (4-hr after dye added) From dam looking up short-arm of pond 11 2/12/951:45 pm (4-hr aner dye added) From dam looking up short-arm of pond 12 2/12/951:45 pm (4-hr after dye added) Picture taken from pier looking at short-arm of pond 13 2/12/951:45 pm (4-hr after dye added) Picture of short-arm of pond taken from top ofhill near pump house 14 2/12/95 2:45 pm (5-hr aner dye added) Picture taken from dam. Short-arm

of pond in foreground. Long-arm of pond in background.

15 2/12/95 2:45 pm (5-hr after dye added) Picture taken from dam. Short-arm of pond in foreground. Long-arm of pond in background.

! 16 2/12/95 2:45 pm (5-hr after dye added) Picture taken from dam. Short-arm of pond in foreground. Long-arm of pond in background.-

17 2/12/95 2:45 pm (5-hr after dye added) Picture taken from dam. Short-arm

, of pond in foreground. Long-arm of pond in background.

I 18 2/12/95 3:45 pm (6-hr after dye added) Picture taken from dam. Looking at boat ramp. Long-arm of pond in background.

, 19 2/12/95 3:45 pm (6-hr after dye added) Picture taken from dam. Looking at boat ramp. Long-arm of pond in background.

20 2/12/95 3:45 pm (6-hr after dye added) Picture taken from boat house roof.

Looking towards boat ramp. Long-arm of pond in background.

21 2/12/95 3:45 pm (6-hr aller dye added) Picture taken from boat house roof.

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1 .ASET: CNPHYTES. DATA CATADSA PLANT

-NORST HEAT TRANSFER- TITLE

~720 71 $ OF HOURS INPUT 20 L1: 8 0F UNIT VOLUME LAYERS 20 K2: SUTPUT CHECK SPACING C

30 S1: 8 0F VERTICAL STAGES IFT)

C C St!:,1): VOLUrf IN POND AT EACH STAGE ( ACFT)

C 0 0 0 0 0 1 1 2 6 10 16 23 32 41 53 66 77 92 113 133 154 176 200 224 251 279 310 341 374 410 C

C St 1,2 ): INITIAL TEMPERATURE AT EACH STAGE (F)

C C2 C2 42 42 42 42 42 42 C2 C2 42 42 42 42 42 42 42 C2 42 42 42 42 42 42 42 C2 42 42 42 42 C

C LtR5 PING VALUES AND PLANT FLCMS FOR TtI,'ll (100G=CU.FT/NR)

C 4 51.4 720 85.7 C

C TII,11: INPUT HEAT IPSTU/HRI C

120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 120 159.3 159.3 142.0 Itt.0 1?,2.0 151.0 151.0 128.5 142.0 128.5142.0 128.5142.0 85.5142.0 77.1 69.9 63.9 59.6 59.6 C

C AtJ) PtJ) MtJ) YtJ) EtJ)

C

%3088341

% 30 C 83 43 33 30 0 83 43 f9 72 2 189 94 91 71 2 198 95 4'372519785 79 71 3 142 81 C3 71 3 166 86 72 61 5 154 73 73 58 3 166 82

[

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3 77 62 4 187 84 ,0 78 63 0 167 80 <

72 66 3 135 77 s 73 69 3 133 78 ,71 77 70 2 157 86 77 63 4 159 80 A*

b L

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1 .TASET: CWHYTES. DATA 72 55 2 131 77 )

74 60 3 155 80 i 77 63 1 153 88 77 65 2 149 84-

• 73 68 3 170 85 76 69 3 149 81-7A 71 2 133 82  :

80 70 3 159 84 l 80 71 3 144 85 i

- C3 72 3 159 84 86 69 3 178 87 88 69 2 190 93 ,

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CA7ApeA -HORST HEAT TOANSFER- ~ PAGE DISC HEAT COUL iM MIXED INTAKE EVAP E K TEN TIM REAL 0984 MIX TEN TEMP AC-FT TCFM TIM TEMP LOSS

-9.8 63.04 12.30 50.74 19 42.00 42.00 0.28 43 ' 83 ; 91 )

$)q) M )eb 1

50.78 19 50.74 12.00 0.60 43 83 86 11 20.2 64.M 13.H 50.78 46.00 0.91 43 83- 86 21 30.6 64.44 13.H 50.78 19 50.78 42.00 1.23 43 83 86 32 41.0 H.44 13.H 50.78 18 83- 86 C2 51.4 H . 44 13. 66 50.78 17 50.78 -42.00 1.56 43 83 M 61.9 6hM_13,HJ.78_.16 GC.78 _42400 1 90__43 E2 86

~3-6 72.3 71.79 20.01 91.79 19 50.78 42.00 1.90 94 189 86 73 82.7 71.79 20.01 91.79 19 91.79 42.00 1.90 94 189 86 84 93.1 70.24 21.40 91.74 18 91.74 42.00 1.90 94 189 86 94 103.5 70.24 22.56 92.80 19 91.74 42.00 1.90 95 198 86 105 114.0 68.55 24.09 92.72 19 92.72 42.00 1.90 95 198 86 115 .124.4 68.55 14.96 90.70 15 90.70 42.00 1.90 85 197 86 89.67 14 89.67 42.00 1.90 85 197 125 134.8 68.55 14.96 88.31 13 88.31 42.00 1.90 81 142 86 136 145.2 68.55 10.25 87.26?12 87.26 42.00 1.90 81 142 86 1% 155.6 68.55 10.25 86.41 42.00 1.90 81 142 86 157 1H .1 68.55 10.25 86.41 11 86.17 10 86.17 42.00 1.90 86 1H 86 167 176.5 68.55 15.15 85.93 9 85.93 42.00 1.90 86.166 86 177 186.9 66.03 17.34 84.86 8 84.86 42.00 1.90 73 154 86 188 197.3 66.03 -5.91 83.93 7 83.93' 50.74 1.90 73 154 86 198 207.7 H .03 -5. 91 83.67 6 63.67 50.78 1.9C 82 166 86 209 218.2 H.73 13.26 5 83.44 50.78 1.90 82 166 86 219 224.6 66.76 13.23 83.44 83.24 4 83.24 50.78 1.90 82 166 86 230 239.0 66.76 13.23 83.24 50.78 1.90 86 163 86 210 249.4 H.76 16.61 83.37 19 83.37 50.78 1.90 86 163 86 -

250 259.8 H.76 16.61 83.20 1 83.37 19 83.20 83.20 1.90 84 187 86 261 270.3 H .76 15.48 85.55 19 83.20 83.20 2.59 84 187 86 271 283.7 99.19 13.H 84.02 19 84.02 83.20 3.21 80 167 86 282 291.1 99.19 16.70 83.51 83.20 3.82 80 167 86 292 301.5 99.19 16.70 83.51 18 83.21 83.20 4.40 80 167 86 303 311.9 97.62 15.33 83.21 17 83.09 83.09 4.87 77 135 86 313 322.4 97.62 16.66 82.98 11 83.09 82.98 82.98 5.34 77 135 86 323 332.8 97.51 16.57 82.93 1 82.93 82.93 5.77 78 133 . 86 334 343.2 97.40 15.58 82.87 1 82.87 82.87 6.21' 78 133 86 3% 353.6 97.34 15.53 82.87 82.87 6.H 86 157 86 355 364.0 97.29~ 9.63 ' 87.H 19 87.H 82.87 7.07 86 157 86 365 374.5 97.19 9.63 87. H 19 85.93 82.87 7.57 80 159- 86 375 384.9 97.29 14.81

't 81 85.93 18 85.07 17 85.07 82.87 8.07 80 159 86 386 3?f.3 97.29 84.55 82.87 8.57 80 159 86 396 400.7 97.29 a .' 84.55 16 86 83.93 15 83.93 82.87 9.08 77 131 407 416.1 95.92 12 ?L 83.48 82.87 9.58. 77 131 86 417 426.6 95.92 1! i1 83.48 14 83.35 82.87 10.12 80 155 86 428 437.0 95.92 13 J 83.35 13 83.24 82.87 10. H 80 155 86 438 447.4 95.92 13.i.) 83.24 12 89.22. 19 83.24 82.87 11.11 88 153 86 448 457.8 95.92 6.70 89.22 82.87 11.55 88 153 86 459 468.2 95.92 6.70 89.22 19 89.22 82.87 12.00 88 153 86 469 478.7 95.92 6.70 89.22 18 88.40 82.87 12.45 84 149 86 480 489.1 95.92 9.99 88.40 17 87.91 .16 87.91 82.87 12.90 84 149 86 '

C90 499.5 95.92 9.99 87.63 82.87 13.35 85 170 86 501 509.9 94.82 8.59 87.63 15 87.43 82.87 13.81 85 170 86 511 520.3 94.82 8.59 87.43 14

-HORST HEAT TRANSFER- PAGE CATAteA DISC HEAT ' COOL . UN MIXED INTAKE EVAP E K TEN TIME REAL TEMP AC-FT TCFM TIME TEFF LOSS D0 bet MIX TEMP 86.90 13 86.90 82.87 14.21 81 149 86 521 530.8 -94.82 11.58 86.50 12 84.50 82.87 14.61 81 149 86 532 541.2 94.82 11.58 86.17 11 86.17~ 82.87 15.01 81 149 86 542 551.6 94.82 11.58 86.02 10 86.02 83.24 15.34 82 ~133 86 553 562.0 94.82 10.29 9 85.90 83.24 15.68 82 133 86 563 572.4 95.19 10.59 85.90 8 85.88 83.24 16.09 84 159 86 573~ 582.9 95.19 9.59 85.88 85.86 83.24 16.50 84 159 86 584 593.3 95.19 9.59 86.37 197 85.86 85.86 83.24 16.91 85 164 86 594 603.7 95.19 8.82 86.32 86.32 83.24 17.30 85 164 86 605 614.1 94.39. 8.12 86.04 19 86.04 83.24 17.65 84 159 86 615 624.5 94.39 8.90 18 85.90 83.24 18.00 84 159 86

.626 635.0 94.39 8.90 85.90 85.85 17 2 85.85 83.24 18.35 84 159 86 636 645.4'94.39 8.90 85.85 8s.85 18.77 87 178 86 CrA 655.8 94.39 6.55 87.84 19 87.84 85.85 19.23 87 178 86 657 666.2 96.99 8.86 - 88.14 19 88.14 85.85 19.71 93 190 86 667 676.6 96.99 3.60 93.39 19 93.39 85.85 20.18 93 190 86 67A 687.1 96.99 3.60 92.48 19 93.39 18 92.48 85.85 20.67 90 194 86 CSS 697.5 96.99 6.34 92.02 17 92.02 85.85 21.16 90 194 86 698 707.9 96.99 6.34 91.75 16 91.75 85.85 21.65 90 194 86

--709 718.3 96.99 6.34 719 728.7 96.99 6.34 91.57 15 91.57 85.85 22.15 90 194 '86.

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