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HomeMy WebLinkAboutNC0004774_Thermal Mixing Zone Modeling Report_20220502 DUKE Duke Energy ENERGY® Buck Combined Cycle 1385 Dukeville Road Salisbury,NC 28146 April 25, 2022 North Carolina Department of Environmental Quality RECEIVED Division of Water Resources MAY* U 2 1617 Mail Service Center 2022 Raleigh NC 27699-1617 NCDEQIDWRINPDES RE: Duke Energy Carolinas, LLC Buck Combined Cycle Station, NPDES Permit NC0004774 Part A. (19.) Clean Water Act Section 316(a) Thermal Variance Dear Sir or Madam: In accordance with the provisions of NPDES Permit NC0004774, Part A. (19.), enclosed is our timely submittal of the requested Clean Water Act § 316(a) information for the Buck Combined Cycle Station. Specifically, the Department has requested that the submitted 316(a) information be provided by April 30, 2022. We believe that this report completely satisfies this obligation. As detailed in the enclosed report, a maximum daily temperature limit of 98°F satisfies the water quality standard within a reasonable distance downstream and allows for safe passage of aquatic organisms. The enclosed report details the model results and defines a plume length for the summer and winter months. Please contact Steve Cahoon (Steve.Cahoon@duke-energy.com, (919) 546-7457 if there are any questions regarding this submittal. Sincerely, ir 4,, l' 11I 1 — Kris Eisenrieth, General Manager II, Buck Combined Cycle Station Attachment: Buck Combined Cycle Station 316(a) Thermal Mixing Zone Modeling Report USPS: 7019 0140 0001 0794 0890 / 9590 9402 5350 9154 1985 45 Thermal Mixing Zone Modeling Report Buck Combined Cycle Station, Salisbury, NC Prepared for: Duke Energy Corporation Charlotte, North Carolina April 13, 2022 Prepared by: Water Environment Consultants Mount Pleasant, South Carolina n 19-44 )14 L_ • ,. • r v � Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station Table of Contents Executive Summary iv 1 Introduction 1 2 Outfall OO1A Discharge Location 3 3 EFDC Modeling 7 3.1 Field Data Collection 7 3.2 Model Setup and Calibration 9 3.3 7Q10 Model Inputs 14 4 Outfall 001A Thermal Mixing Zone Results 19 5 Permit Recommendations 22 6 References 23 r : ii °v `�'' Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station List of Figures Figure 1-1. Site Location Map(not current aerial imagery) 2 Figure 2-1. Outfall 001A discharge—August 14, 2019 4 Figure 2-2. Outfall 001A and wingwall—August 14, 2019 5 Figure 2-3. Shoal and small channel along upstream side of wingwall (photo taken August 14,2019) 6 Figure 2-4. Wingwall Breach connecting channel at property bulkhead(photo taken August 14, 2019) 6 Figure 3-1. River depths measured on August 14, 2019 (aerial dated February 3, 2018,shows higher flow conditions) 8 Figure 3-2. Measured velocities(depth-averaged)on August 14,2019(aerial dated February 3,2018, shows higher flow conditions) 8 Figure 3-3. EFDC model grid 10 Figure 3-4. EFDC model grid depths 11 Figure 3-5. Model grid and bathymetry converted to feet relative to NAVD88 12 Figure 3-6. Calibrated model and measured current velocities(upstream study area) 13 Figure 3-7. Calibrated model and measured current velocities(downstream study area) 14 Figure 3-8. Location of USGS station and catchment basins in relation to the project site. 16 Figure 3-9. Flow-stage relationship at USGS station 02116500 17 Figure 4-1. Summer 7Q10 thermal plume model results and 89.6°F standard mixing zone 20 Figure 4-2. Summer 7Q10 thermal plume model results and 5.04°F(delta-T)standard mixing zone 20 Figure 4-3. Winter 7Q10 thermal plume model results and 5.04°F(delta-T)standard mixing zone 21 List of Tables Table 3-1. 7Q10 flow determination 16 Table 3-2. 7Q10 model water level adjustments 17 Table 3-3. 7Q10 model inputs 18 _�[ X_j t 1. v 'LAC'"., Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station Executive Summary Duke Energy Corporation (Duke) retained Water Environment Consultants(WEC)to prepare this report for submission to the North Carolina Department of Environmental Quality(NCDEQ) in support of existing NPDES permit NC0004774. Duke owns and operates the Buck Combined Cycle Station (Buck), located in Salisbury, NC along the Yadkin River. In early 2019, Duke retained WEC to collect field data within the Yadkin River and conduct a thermal mixing model of Buck's effluent discharge. WEC recorded field measurements in August 2019, and in accordance with the original project scope,WEC investigated the feasibility of conducting a thermal mixing model using CORMIX. Given the irregularities of the site conditions, particularly around the discharge outfall, an accurate model of the effluent and river mixing necessitated a different approach. Subsequently,WEC recommended using a two-dimensional application of the Environmental Fluid Dynamic Code (EFDC) model instead,and Duke submitted a WEC- prepared Thermal Modeling Study Plan(WEC 2021)to NCDEQ for approval. This report summarizes the EFDC mixing zone model analysis and demonstrates that the proposed limitations and thermal mixing zone meet the state surface water standards for temperature. Buck's coal-fired steam station is retired,and all power is now generated at the Combustion Turbine Combined Cycle (CTCC) plant. Under permit NC0004774, Duke's steam station discharged 395 million gallons per day(MGD) of once-through noncontact cooling waters to the mainstem of the Yadkin River. The new CTCC plant generates a drastically reduced thermal discharge,estimated to total 0.62 MGD, which flows through Outfall 001A into the Yadkin River. This section of the Yadkin River is categorized by NCDEQ as Lower Piedmont(15A NCAC 02B .0202, Definitions)and is classified WS-V(also protected for Class C uses). The NCDEQ water quality standard for temperature has two components: not to exceed 2.8°C(5.04°F)above natural background (referred to herein as the delta-T standard)and not to exceed 32°C(89.6°F) (i.e.,the maximum standard). Both conditions must be met at an acceptable distance downstream while also allowing safe passage of aquatic organisms. WEC set up the EFDC model using the water depths and water surface elevations measured in the field. The model was calibrated to the field-measured currents. Once calibrated,the model was used to evaluate mixing and dilution of the discharge plume within the Yadkin River under critical 7Q10 flow. While this analysis does not consider heat loss to the atmosphere(a conservative assumption), it does include summer and winter ambient water temperatures in addition to the seasonal 7Q10 (the lowest 7- day average flow that occurs [on average] once every 10 years)flows. Results from this mixing zone analysis indicate a year-round, daily maximum temperature limit of 98.0°F satisfies the water quality temperature standards within a reasonable distance downstream and allows safe passage of aquatic organisms. For the summer 7Q10 model,the maximum and delta-T standards are met at thermal plume lengths of 204 feet and 266 feet, respectively. For the winter conditions model,the delta-T standard is met at a plume length of 224 feet. Because the ambient water temperature is cooler in the winter,the thermal plume dilutes below the 89.6°F maximum standard faster than during summer(i.e.,the winter plume is smaller than the summer). In all cases,the cross- L � iv Thermal Mixing Zone Modeling Report—Buck Combined Cycle Station shore plume width does not extend beyond the end of the wingwall, and thus,the thermal plume will not inhibit the safe passage of aquatic organisms. Because the thermal mixing zone established by this conservative modeling analysis satisfies both temperature standards,continuation of the Clean Water Act(CWA) 316(a)thermal variance is not necessary. Therefore, Duke may request a permit modification that includes the annual 98.0°F discharge limit and eliminates the CWA 316(a)thermal variance. Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station 1 Introduction Duke Energy Corporation (Duke) retained Water Environment Consultants(WEC)to prepare this report for submission to the North Carolina Department of Environmental Quality(NCDEQ) in support of existing NPDES permit NC0004774. This report summarizes a thermal mixing zone analysis for Duke's Buck Combined Cycle Station (Buck), located in Salisbury, NC(Figure 1-1). Buck's coal-fired steam station is retired,and all power is now generated at the Combustion Turbine Combined Cycle (CTCC) plant. Under permit NC0004774, Duke's CTCC plant discharges an estimated 0.62 million gallons per day(MGD)to the Yadkin River through Outfall 001A. WEC developed an application of the Environmental Fluid Dynamics Code (EFDC) model to simulate thermal mixing of the heated effluent with the ambient waters of the Yadkin River. This analysis can be used to propose a new,year-round temperature limit for Duke's Buck station and remove the Clean Water Act(CWA) 316(a) requirement from the existing permit. The model results also indicate the size of the mixing zone needed to satisfy state water quality standards for temperature and that also allows for safe passage of aquatic organisms. WEC's analysis to support these conclusions is provided in the following sections: • Section 2, Outfall 001A Discharge Location—provides a brief description of the outfall location; • Section 3, EFDC Modeling—describes the field data collection, model setup and calibration, and 7Q10 modeling application; • Section 4, Outfall 001A Thermal Mixing Zone Results; and • Section 5, Permit Recommendations. rar 1 11.: Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station a scam 444 Otitfal[ 001A .xx e , �, i•, „b yam, 'r _ _._.. _�"� .._. ,. - ,.. A o 250 500 1,000 Fee Figure 1-1. Site Location Map(not current aerial imagery) 2 Thermal Mixing Zone Modeling Report—Buck Combined Cycle Station 2 Outfall OO1A Discharge Location As previously mentioned,the site's coal-fired steam station is retired,and all power is now generated at the CTCC plant. Heated effluent from the CTCC plant discharges from Outfall OO1A into the mainstem Yadkin River via a downward facing pipe along the property bulkhead (Figure 2-1). The outfall location is impounded by a wingwall that extends from the shore, slightly upstream of the discharge, into the river parallel to the shoreline (Figure 2-2). The wingwall is exposed during critical, low-flow, 7010 scenarios, effectively separating the ambient waters of the Yadkin River from the heated effluent at Outfall 001A. Where the wingwall meets the property bulkhead,the upper portion of the wingwall was breached so that the area contained within the wingwall is partially connected to the ambient waters upstream of the discharge. This partial connection occurs via a small channel that has formed along the upstream side of the wingwall, between the wall and a sandy shoal. Figures 2-3 and 2-4 show photos of the wingwall breach,the small channel, and shoal. 3 L'..�' Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station I t 81 .4.1111 t"' ' 4 T , , , , m4 e... y fi. Figure 2-1. Outfall 001A discharge—August 14,2019 Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station ti , tea« v. 41,1 f Flow Direction __. .n,� .. t.,° ri r 101A Wingwall o extends to shore '2 Figure 2-2. Outfall OO1A and wingwall—August 14, 2019 Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station • illit '' I ' ' \' Figure 2-3. Shoal and small channel along upstream side of wingwall (photo taken August 14, 2019) , 4 tilkIL r . _ ' - .- ;,' •-py.e4S:,"' ;LT Figure 2-4. Wingwall Breach connecting channel at property bulkhead(photo taken August 14,2019) in v L-- -_ ' 6 Thermal Mixing Zone Modeling Report—Buck Combined Cycle Station 3 EFDC Modeling This portion of the Yadkin River is categorized as Lower Piedmont(15A NCAC 02B .0202, Definitions) and is classified WS-V(also protected for Class C uses). The NCDEQ water quality standard for temperature has two components: not to exceed 2.8°C(5.04°F)above natural background (referred to herein as the delta-T standard) and not to exceed 32°C(89.6°F) (i.e.,the maximum standard) (15A NCAC 02B.0211 Fresh Water Quality Standards for Class C Waters). Both conditions must be met at an acceptable distance downstream while also allowing safe passage of aquatic organisms. The purpose of the model study is to simulate the thermal mixing of the effluent wastewater with the ambient river flow and determine if the discharge will meet these standards. The study results may be used to propose a new, year-round temperature limit for Duke's Buck Station and remove the CWA 316(a) requirement from the existing permit. The following subsections describe: 1)field data collected to support the model, 2) model setup and calibration, and 3) inputs used for modeling under 7Q10 conditions. 3.1 Field Data Collection To develop a model that demonstrates compliance with the NCDEQ water quality standards for surface water temperature,WEC collected field data including detailed measurements of current velocities, water depths,and water surface elevations. These data were necessary for model setup and calibration. Field measurements were recorded on August 14, 2019,when the river was at a low-flow condition, as close to 7Q10 conditions as possible. The study area extended from just upstream of Outfall 001A to approximately 1,800 feet downstream. While the river flow rate during the field measurements is discussed below, please refer to Section 3.3 for discussion of 7Q10 conditions. Water depth data were required to create a two-dimensional grid for the EFDC model. Measured water surface elevations along the river were used to convert the depths to bottom elevations relative to a fixed vertical datum. Current velocity measurements were required for comparison to the modeled currents to verify that the model reasonably represents the hydrodynamics in the river. WEC used a Sontek RiverSurveyor-M9 to collect water depths and current velocities within the Yadkin River. The RiverSurveyor-M9 is an Acoustic Doppler Current Profiler(ADCP)that is equipped with a differential GPS that provides horizontal positioning data. The ADCP measures depths and currents through the water column as it traverses the river, providing a two-dimensional cross-section of current velocities. Figure 3-1 shows the measured water depths along the ADCP transect paths. Figure 3-2 shows the depth-averaged current velocities. These velocities were scaled to a common reference magnitude in both length and color. The arrows indicated flow direction and were anchored at the point of measurement(i.e.,the arrow's base). The average river flow rate calculated by the ADCP was 54 cubic meters per second (m3/s)or 1,903 cubic feet per second (ft3/s). Water surface elevations were measured using a Trimble Geo 7x Centimeter Edition GPS,capable of ±0.1-foot accuracy. WEC used the data to convert the measured water depths to bottom elevations relative to the North American Vertical Datum of 1988(NAVD88). These bottom elevations were later interpolated onto the model grid as discussed below. The water surface elevation during data collection was measured as 189.3 meters NAVD88 (620.9 feet NAVD88). Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station �Outfall 001A "' � 1 7 . . k Legend '' Measured Depths (ft) 10.1 - 12.0 I ,. '" • < 20 - 12.1 - 14.0 1 ' ." '''' ,., fiy.' . • 2.1 -4.0 14.1 - 16.0 A _.__. -.__ ' N. 4.1 -6.0 16.1 - 18.0 0 125 250 500 6.1 8.0 • 18.1 20.0 Feet � - 8.1 10.0 • > 20.0 Figure 3-1. River depths measured on August 14, 2019 (aerial dated February 3,2018, shows higher flow conditions) J .' Figure 3-2. Measured velocities(depth-averaged) on August 14,2019(aerial dated February 3,2018, shows higher flow conditions) Thermal Mixing Zone Modeling Report—Buck Combined Cycle Station 3.2 Model Setup and Calibration WEC created a two-dimensional model grid of the Yadkin River, beginning just upstream of Outfall 001A and extending approximately 1,800 ft downstream (Figure 3-3). The grid was comprised of 12,526 cells. These cells were mostly uniform,2-meters by 2-meters in size. The wingwall was accounted for in the model grid by de-activating the model cells that overlapped the wall location. Deactivated cells were effectively removed from the model calculations blocking flow from passing through these cells. The model domain included eleven active grid cells between the shoreline and the end of the wingwall to resolve flow patterns in the sheltered region behind the wall. The field-measured water depths and bathymetry were interpolated onto the model grid, illustrated in Figure 3-4 and Figure 3-5. As noted during the field measurements and discussed above,the grid bathymetry included the small channel and shoal along the upstream side of the wingwall. The breach in the wall was included in the model. While high flow events could alter the shoal and shallow channel, historical imagery and vegetation growth suggests the shoal has remained stable. Boundary conditions for the calibration model included the river flow at the upstream boundary and the measured water surface elevation at the downstream boundary. The ADCP measured flow within the Yadkin River was distributed across the upstream grid cells. The effluent discharge rate was included in the calibration model within the grid cell corresponding to Outfall 001A. Duke provided a timeseries of Outfall 001A effluent flow rates that coincided with field measurements collection. The downstream boundary was specified as an open boundary,set to the field-measured water surface elevation. To confirm the EFDC model hydrodynamics,WEC compared the modeled and measured currents to evaluate agreement in current magnitude and direction. Figure 3-6 and Figure 3-7 illustrate the modeled and measured current velocities in feet per second (ft/s). In these figures,the field measured currents are indicated by the red node. Both modeled and measured velocity vectors indicate flow direction and are scaled to a common magnitude in color and length. Overall,the modeled currents are in reasonably good agreement with the measured velocities,and the model is sufficiently calibrated in this area for the purposes of evaluating the spatial extent of the discharge mixing zones. Results from hydrodynamic model are typically smoother and show less variation than direct measurements in rivers. The model is a snapshot in time whereas the field- measured currents took place over several hours. Because the Yadkin River flow rate fluctuated slightly over the course of field measurements,the model was expected to show some differences from the measured data. For instance,the model does not show the isolated, individual peaks in currents in the center of the river(as shown by the yellow vectors in Figure 3-6). This area of the river does not affect flows behind the wingwall or near Outfall OO1A,though. In contrast,the model accurately demonstrates an eddy formation on the leeward side of the wingwall as captured in field measurements. As mentioned in the Study Plan (WEC 2021), WEC modeled dilution of the Outfall 001A effluent plume through advection only and did not include a full thermal model with heat loss from the water column -p 9 Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station n { .1", Outfall 001A' " r l d r 1 1 - 1 1 • 1 / .... _.i...L.. '':_, �' '�. Y , .` „ " . '''''. ,A t, 0 DSO 500 Legend IMENIVIIIIIIIIII Feet .. Model Grid t. 100,"..o101144. Figure 3-3. EFDC model grid to the atmosphere. This is a conservative approach, and since a full thermal model was not conducted, the model did not need to be calibrated for temperature. For a dilution analysis,the primary calibration factors are current patterns and the dispersion coefficient. As a conservative assumption, WEC set the dispersion coefficient to zero and based dilution only on advection. _. _ 10 =,& Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station rL ' ___._ .- H-_1.J. - _ ` 'I `"Outfall 001 . -& ,,- M ' ., maw.:. �.a.F '' I 1 < _ I, Legend r ; -::_ '"*-- 1" Lill, Depth (ft) 10.1 - 12.0 '.»e 4 ,` r '0:; - t 0.2 - 2.0 12.1 - 14.0 2.1 -4.0 14.1 - 16.0 �< 4.1 - 6.0 16.1 - 18.0\ 1 .. r A 0 125 250 500 6.1 - 8.0 18.1 - 20.0 Feet1 8 1 - 10 0 > 20 0 Figure 3-4. EFDC model grid depths --. — ✓ 11 Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station r� 'q '' , d7 i„7 lag. ,�ry A f l \Outfa!'001 ,� Legend f + i� Bottom Elev (ft NAVD88) 610.1 -612.0 ►, <i ' ® 600.5 602.0 612.1 614.0 r.a� R 602.1 604.0 614.1 -616.0 . . .;. .,. r R 604.1 606.0 616.1 618.0 0 125 250 500 606.1 608.0 618.1 -620.0 A Fee �.. 620.1-. 608.1 -610.0 622.0 Figure 3-5. Model grid and bathymetry converted to feet relative to NAVD88 r 12 Thermal Mixing Zone Modeling Report—Buck Combined Cycle Station //��Y yy�� � � i *ice'• •t:.:�, wy "Ve�?,J:k ��(,,,�- 0.47 `� Ys g! x ARw � q. �T"xn.waM , '9xxd „fM'a my^:S, off x' 1.0 - - — — • - .x - w ..a• "" ,.. �... a a . .,a '.,'` - ....wp' - ,,r,',�,•..—,r!'"w'' ...;,r'. ,we, • i4 .. = "C s. .. - Y aaa 7,.. c;* - �,. �_ .. - • r � ,. are ; � .fi'1'"`'^m"-'.,�,•' -,- . -• _. '�}� � �,,.� are - _ ,., a . " " �..-z..a .�.we w -¢4 w Figure 3-6. Calibrated model and measured current velocities (upstream study area) 1--"1 13 Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station k/ ,qp N. r bqz V I0 t • r,r Figure 3-7. Calibrated model and measured current velocities (downstream study area) 3.3 7Q10 Model Input As outlined in the Study Plan (WEC 2021), for this analysis, a 98.0°F daily maximum effluent temperature was evaluated. The 98.0°F was determined by adding a minimal 3.0°F compliance margin to the existing 95.0°F permitted temperature limit. As done in other NCDEQ approved mixing zone models for Duke, this compliance margin was determined to be a reasonable balance between the daily variability of grab samples (versus a monthly limit and/or continuous temperature measurement) and a slightly larger permitted mixing zone caused by the 3.0°F. Summer and winter ambient temperature conditions were considered to ensure compliance throughout the year. WEC defined summer months as March through October and winter months as November through February for the seasonal models as conservative model inputs. These months reduce the ambient temperatures,therefore maximizing the temperature difference between or"excess" (i.e.,the effluent temperature above ambient). The EFDC model was run under two conservative assumptions: maximum permitted discharge rate of 0.62 MGD and temperature dilution from mixing only(i.e., no heat exchange with the atmosphere). Adjusted inputs for this mixing zone analysis included the summer and winter ambient 7Q10 flow rates, the downstream water surface elevation, and inclusion of the permitted discharge flow rate. The discharge thermalplume was evaluated byinputting an effluent "dye" concentration to the g P g Y temperature excess at Outfall 001A. 14 Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station The original 7Q10 flow rate at the project site was determined in the 1980's and is outdated. In 2016, however,the U.S. Geological Survey(USGS) published updated flow rates for upstream gauge stations using data through 2012 (Weaver 2016). The appropriate 7010 flow rate for input to the model must consider that the Yadkin River bifurcates and flows around an island at the project site, as seen in Figure 1-1, and the model domain is limited to the river channel on the south side of the island. WEC estimated 7010 flow at the project site using two methods and used the more conservative (lowest)value for the mixing analysis. The first method was to use 99%of the 2016 published summer and winter 7010 values at the upstream USGS station 02116500. The 99%fraction was determined as the ratio of WEC-measured flows of the south channel (1,903 cfs) and the reported flow during that time at the USGS station (1,929 cfs). The second method of determining 7010 flow was to add the incremental inflow between the USGS station and the project site to the published 7Q10 values, proportional to the additional watershed area. This total river flow was split around the island based on the relative channel widths on the north and south sides of the island. Based on channel widths, approximately 71%of the total flow remains on the Buck Station (southern)side of the river. Figure 3-8 shows the location of Buck Station, USGS station 02116500,and the respective watershed basins as determined from USGS StreamStats(USGS 2019). Table 3-1 summarizes the results of the two methods. The more conservative (lowest) results and the 7Q10 rates used for this analysis are 536 ft3/s and 1,006 ft3/s for summer and winter, respectively,which were determined using the first method described above. The water surface elevation input to the model boundary was lowered from recorded field measurements based on the change in water depths at USGS station 02116500 associated with similar changes in flow rates. Figure 3-9 shows the measured depths and flow rate data at the USGS station (USGS 2022). Based on a best-fit equation of this data developed by WEC, and similar stream characteristics at both sites,WEC determined the water levels(or stage)at the project site associated with the summer and winter 7010 flow rates. For the summer 7Q10 condition,the field-measured water surface elevation was lowered by 1.1 ft(0.3 m),the difference between the stage elevations during the 7Q10 flow and the flow during field measurements. For the winter 7010 condition,the measured water level was lowered by 0.7 ft(0.2 m). Table 3-2 summarizes these adjustments. The resulting 7010 water surface elevations at the downstream model boundary were 188.9 meters NAVD88 (619.8 feet NAVD88)for the summer model and 189.0 meters NAVD88(620.2 feet NAVD88)for the winter model. Thermal mixing from the Outfall 001A discharge was modeled using EFDC's dye tracer module. This method simulates thermal dilution from mixing only,excluding heat losses to the atmosphere as previously mentioned, providing a conservative analysis. As the warm effluent mixes with the cooler ambient waters of the Yadkin River,the excess temperature of the plume dilutes. WEC then identified the downstream points where the plume dilution satisfied both the maximum and delta-T temperature standards. v L \.� 15 Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station State F USGS Basin Area:2280 mi2 Project Site Basin Area: 3452 mi2 v'nsto Sate u USGS 02116500 Yadkin River at High Pole t• Yadkin College, NC it-, di. .,.,,,F,,I Legend it II * name * Project Site rt r AO- USGS Station N 0 5 10 20 I I USGS Station Basin Miles Q Project Site Basin Figure 3-8. Location of USGS station and catchment basins in relation to the project site. Table 3-1. 7Q10 flow determination Variable: Value 7010 flow—Summer(USGS 02116500): 543 ft3/s 7Q10 flow—Winter(USGS 02116500): 1,020 ft3/s Method 1 Average Measured Flow(August 14,2019): 1,903 ft3/s Average USGS flow 12 AM-12 PM (August 14,2019): 1,929 ft3/s Ratio of Measured to USGS Data: 99% 7Q10 flow—Summer: 536 ft3/s 7010 flow—Winter: 1,006 ft3/s Method 2 Incremental Drainage Area: 1,172 mi2 incremental 7010 flow—Summer: 279 ft3/s incremental 7010 flow—Winter: 524 ft3/s 71%x(7Q10+ incremental inflow)—Summer: 584 ft3/s 71%x(7Q10+ incremental inflow)—Winter: 1,097 ft3/s 16 L Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station Stage vs. Flow Rate 645 • USGS Data 644 • 7Q10-summer 643 7Q10-winter 642 • Field Days I 00 • 0 638 637 R2=100 636 635 0 500 1000 1500 2000 2500 3000 3500 4000 4500 5000 Flow(ft3s) Figure 3-9. Flow-stage relationship at USGS station 02116500 Table 3-2. 7Q10 model water level adjustments 7Q10-summer 7Q10-winter 8/14/2019 Flow(ft3/s): 536 1,006 1,903 USGS Station Stage(ft NAVD88): 638.4 638.8 639.5 Delta,as compared to 8/14/2019(ft): 1.1 0.7 Adjusted Stage,from field-measured 619.8 620.2 620.9(ft NAVD88): WEC reviewed monitoring data from NCDEQ's Ambient Monitoring System on the Yadkin River,Station Q4660000 just upstream of Buck,to determine the modeled ambient river temperatures during summer and winter conditions (Water Quality Portal 2022). During the summer months, WEC analyzed the 95th percentile ambient temperature (83.9°F)for compliance with the 89.6°F maximum standard. The 95th percentile is used because it will take longer for the effluent to meet the maximum standard when the ambient water is warm as compared to when it is cold (e.g., the 5th percentile). With a temperature excess of 14.1°F(98.0°F minus 83.9°F),this standard is met once the plume excess dilutes to 5.7°F (83.9°F+5.7°F=89.6°F). For compliance with the 5.04°F delta-T standard during summer months,WEC analyzed the 5th percentile ambient temperature (50.0°F). This standard is met once the plume excess dilutes to 5.04°F.The difference in the ambient and effluent temperatures is greater during winter months than during summer. The thermal plume during the winter months will dilute below the 89.6°F maximum standard at a shorter distance from Outfall 001A than during the summer months, even under the warmest, ambient winter temperatures. Therefore, summer conditions were modeled to for determine the worst-case scenario for compliance with the 89.6°F maximum standard. ►.:kir .�� 17 Thermal Mixing Zone Modeling Report — Buck Combined Cycle Station Because the temperature excesses are greater than when evaluating against the maximum standard, and will take longer to dilute downstream, it is more critical to examine where the delta-T standard is met. WEC analyzed the 5th percentile ambient temperature during the summer and winter months,for compliance with the 5.04°F delta-T standard. It is obvious that because the temperature excess is greater in the winter, it will be the critical condition for determining compliance with the 5.04°F delta-T standard. Table 3-3 summarizes the 7Q10 model inputs. Table 3-3. 7Q10 model inputs Variable Summer Model Winter Model 7Q10 Flow Rate (m3/s): 15.2 (536 cfs) 28.5 (1,006 cfs) Downstream Water Level (m NAVD88): 188.9 (619.8 ft) 189.0(620.2 ft) Effluent Flow Rate (m3/s): 0.027 (0.62 MGD) 0.027 (0.62 MGD) Effluent Temperature (°F) 98.0 98.0 95th Percentile Ambient Temperature (°F) 83.9 51.4 95th Percentile Temperature/"Dye" Concentration: 14.1 - 5`h Percentile Ambient Temperature (°F) 50.0 33.3 5th Percentile Temperature/"Dye" Concentration: 48.0 64.7 T r 18 Thermal Mixing Zone Modeling Report—Buck Combined Cycle Station 4 Outfal1001A Thermal Mixing Zone Results The EFDC model was executed for a four-day simulation period,ample time for plume and hydrodynamics to reach steady-state given the constant input boundary conditions. Figures 4-1 and 4-2 show the model results for the 0.62 MGD, 98.0°F discharge during the summer conditions for the maximum and delta-T standards, respectively. Figure 4-3 shows model results for the winter condition delta-T scenario. The color contours represent the thermal plume's temperature excess above background in degrees Fahrenheit. In each plot,the dark red color represents the portion of the plume that exceeds the temperature standard,for the 89.6°F maximum and 5.04°F delta-T standard. Thus,the edge of the dark red delineates where the temperature standards are met. In the summer conditions model,the 89.6°F maximum standard is met with a thermal plume length of 204 ft. Also,the summer conditions model 5.04°F (delta-T)standard is met with a plume length of 266 ft. In the winter model,the 5.04°F (delta-T)standard is met with a plume length of 224 ft. At the downstream end of the wingwall,an eddy causes the discharge plume to recirculate behind the wall and slowly mix with the ambient river flow. As a result,the cross-stream width of the thermal plume does not extend beyond the end of the wingwall (approximately 27 percent of the river width), and it would therefore allow safe passage for aquatic organisms that may be inhibited by a slight increase in temperature. 19 Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station ION" 4'it 'x it.rt . 41';•-•"'nil r Legend * Outfall 001A 2.1 -3-0 Temperature Excess(°F) 3.1 -4 0 » i» � � 0.0-0.1 4.1 -5.0 z 0 125 250 500 ` °'u`~ 0.1 - 1.0 5 1 -5 7 :. A Feet g ) 1.1 -2.0 >5.7 r Figure 4-1. Summer 7Q10 thermal plume model results and 89.6°F standard mixing zone 1 arm jn I ,Lr� ;' ' r ' " 1:4 • ems-' . , - Legend • Outfall 001A 1 01 -2 00 ,, " ""' "' Temperature Excess(OF) 2-01 -3.00 a ,; - 00-001 301 -400 ' Ak 0 125 250 500 111111 0.01 -0 50 4 01 -5.04 Feet _ 0.51 1.00 >5 04 . - —_u .^st... Figure 4-2. Summer 7Q10 thermal plume model results and 5.04°F (delta-T) standard mixing zone 20 • V L' - - Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station Legend • Outfall 001 A 1.01 -2.00 .• Temperature Excess(°F) 2.01 -3.00 •,., 0.0-0.01 3.01 -4.00 A0 125 250 500 0.01 -0.50 4.01 -5.04 Feet 0.51 - 1.00 >5.04 Figure 4-3. Winter 7Q10 thermal plume model results and 5.04°F (delta-T) standard mixing zone ` ArL 21 Thermal Mixing Zone Modeling Report—Buck Combined Cycle Station 5 Permit Recommendations Results of this modeling study indicate that a year-round 98.0°F thermal discharge would satisfy both conditions of the NCDEQ water quality standards for temperature at a short distance downstream. The plume size allows for safe passage of aquatic organisms,as the plume is confined to a small area adjacent to the bank and does not extend across the river. Results from this analysis support Duke's request for a year-round, daily maximum temperature limit of 98.0°F. Of course,the thermal plume will be even smaller than what these conservative models predict because 1)actual discharge temperatures and flow rate will be less than the maximum permit limits,and 2)this analysis considers extreme ambient temperatures(both high and low) and excludes atmospheric heat loss. Because the actual temperature excess will be far less and likely immeasurable within the DEQ-approved mixing zone,these conservative models prove that instream monitoring/limit should not be required. Finally, because the permit will include approval of this relatively small thermal mixing zone,continuation of the 316(a) temperature variance should not be necessary,and this requirement may be removed from the NPDES permit. A L� 22 Thermal Mixing Zone Modeling Report-Buck Combined Cycle Station 6 References EPA 2021. https://www.epa.gov/ceam/environmental-fluid-dynamics-code-efdc. Accessed July 21, 2021. Hill, David. "RE: [EXTERNAL] Duke Energy Buck Combined Cycle Plan Thermal Modeling". Correspondence with NCDENR and Duke Energy. December 7,2021. E-mail. USGS. 2019.StreamStats: Streamflow Statistics and Spatial Analysis Tools for Water-Resources Applications. March 4, 2019,accessed 2022 at https://www.usgs.gov/mission-areas/water- resources/science/streamstats-streamflow-statistics-and-spatial-analysis-tools USGS. 2022. National Water Information System. USGS 02116500 Yadkin River at Yadkin College, NC. Water Data for the Nation,accessed 2022 at https://waterdata.usgs.gov/nwis/uv?site no=02116500 Water Quality Portal. 2022. National Water Quality Monitoring Council.Yadkin Riv at HWY 150 NR Spencer(21NC01WQ-Q4660000)site data in the Water Quality Portal.accessed 2022 at https://www.waterqualitydata.us/provider/STORET/21NC01WQ/21 NC01WQ-Q4660000/ Weaver C.J. 2016. Low-Flow Characteristics and Flow-Duration Statistics for Selected USGS Continuous- Record Streamgaging Stations in North Carolina Through 2012.Scientific Investigations Report 2015-5001.Version 1.1, March 2016. Prepared in cooperation with the North Carolina Department of Environment and Natural Resources, Division of Water Resources. WEC. 2021.Thermal Model Study Plan. Buck Combined Cycle Station,Salisbury, NC.July 30, 2021. Prepared for Duke Energy Corporation, Charlotte, NC. r 23