Title: An Analytical Screening Technique to Estimate the Effect of Cooling Ponds on Meteorological Measurements
1An Analytical Screening Technique to Estimate the
Effect of Cooling Ponds on Meteorological
Measurements A Case Study
- Stephen A. Vigeant, CCM and Carl A. Mazzola, CCM
- Shaw Environmental Infrastructure
PAMS Mini-Conference, Columbia, SC April 3, 2009
2Outline
- Introduction
- Study Objective
- Technical Approach
- Sensible heat and moisture flux source terms
- Atmospheric transport and diffusion
- Results
- Conclusions
3Introduction
- Situation Overseas nuclear power station
meteorological monitoring program with 2
instrumented towers (58-meter 10-meter) - Cooling system Includes two 12 m x 12 m cooling
ponds with elevated water temperatures - Ponds Located 62 meters from 10-meter tower
instrumentation - Issue Nuclear regulatory agency concerned about
possible effects of cooling ponds on 10-meter
tower measurements
4Study Objective
- Develop analytical technique to estimate
potential impact of cooling ponds on 10-meter
tower temperature and RH measurements - Source Terms Estimate sensible heat and moisture
fluxes from cooling ponds - Atmospheric Transport and Diffusion Determine
impacts of fluxes on 10-meter tower measurements
using appropriate model - Use 1-year of onsite data to estimate source term
and atmospheric transport and diffusion - Calculate temperature and moisture impacts to
10-meter tower instrumentation
5Technical ApproachSensible Heat and Moisture
Fluxes
- Bulk aerodynamic formulae of Friehe and Schmitt
(1976) selected to estimate sensible heat and
moisture fluxes from cooling ponds - Fluxes primarily driven by
- Water and air temperature differences
- Wind speed above ponds
6Sensible Heat and Moisture Fluxes
Wind
Sensible Heat Moisture Fluxes
Ta
Discharge Pond Ts
7Technical ApproachSensible Heat and Moisture
Fluxes
- Sensible Heat Flux Hs rCpCHU(Ts Ta)
- where
- Hs sensible heat flux (cal m-2 sec-1)
- r air density (g m-3)
- Cp heat capacity of air (cal g-1 K-1)
- CH sensible heat transfer coefficient
(dimensionless) - U mean wind speed (m sec-1) at reference
height (10 meters) - Ts mean water temperature (K)
- Ta mean air temperature at reference height
(10 meters) (K)
8Technical ApproachSensible Heat and Moisture
Fluxes
- Moisture Flux E CeU(Qs Qa)
- where
- E moisture flux (g m-2 sec-1)
- Ce moisture transfer coefficient
(dimensionless) - U mean wind speed (m sec-1) at reference
height (10 meters) - Qs mean water vapor density (g/m3) near the
water surface - (assume saturation)
- Qa mean water vapor density (g/m3) at reference
height - (10 meters)
9Technical ApproachSensible Heat and Moisture
Fluxes
- Water vapor densities (Qs and Qa)
- Qs and Qa r?(RH x Ws) / (1 RH x Ws)
- where
- r air density (g m-3)
- Ws saturation mixing ratio (dimensionless)
- RH relative humidity (dimensionless)
- Qs (based on water temperature)
- Qa (based on air temperature)
10Technical ApproachSensible Heat and Moisture
Flux Source Terms
- Calculate hourly sensible heat and moisture
fluxes using one year of onsite measurements - Base sensible heat transfer coefficients (CH) on
seasonal values obtained from site-specific study
- Base moisture transfer coefficient (Ce) on Friehe
Schmitt - Use seasonal intake water temperature
measurements - Assume pond temperature is 7C higher
- Assume flux homogeneity over entire pond surface
- Multiply calculated fluxes (cal m-2 sec-1 g m-2
sec-1) by pond surface area - Obtain sensible heat and moisture source terms
(cal sec-1 g sec-1)
11Technical ApproachAtmospheric Transport and
Diffusion
- Determine transport and diffusion of sensible
heat and moisture source terms - Calculate normalized concentrations (C/Qs) at
10-meter tower located 62 meters from cooling
ponds - Use NRC ARCON96 code due to close proximity of
source and receptor - Horizontal and vertical diffusion coefficients
adjusted for plume meander and aerodynamic
building wake - Empirical adjustments based on many wind tunnel
and atmospheric tracer studies - NUREG/CR-6331 Revision 1
- Use hourly onsite data from 10-m tower ARCON96
input
12Technical ApproachAtmospheric Transport and
Diffusion
- ARCON96 Code Description
- Straight-line Eulerian Gaussian plume
- Ground-level, vent, and elevated releases
- Incorporates low wind speed plume meander
- Incorporates aerodynamic building wake effects
- Valid at source-receptor distances as close as 10
meters - Recommended by NRC for use in control room
habitability analyses in Regulatory Guide 1.194
13Technical ApproachAtmospheric Transport and
Diffusion
- ARCON96 Code Input Options
- Area source (virtual point) option used for
cooling ponds - Sector averaging constant (4.3)
- Wind direction sector width (90 degrees azimuth)
- Surface roughness length (0.2 m)
- One year of hourly onsite meteorological data
14Technical Approach Sensible Heat and Moisture
Concentrations
- Multiply sensible heat (cal sec-1) and moisture
(g sec-1) fluxes by calculated ARCON96 C/Q values
(sec m-3) - Obtain hourly values of sensible heat (XH) (cal
m-3) and moisture concentration (Xw) (g m-3) at
10-m tower instruments - XH Hs (C/Q) Sensible Heat Concentration
-
- XW E (C/Q) Water Vapor Concentration
15Technical ApproachPond Sensible Heat and
Moisture Impact Calculations
-
- Calculate increase in temperature (DTa) at
10-meter tower - DTa XH/Cpr
- Calculate increase in RH (DRH) at 10-meter tower
- DRH 100 x XW (g m-3) / rW (g m-3)
16Results
- Temperature Impact
- Largest hourly temperature impact 0.2C
- Increase between 0.10C - 0.19C (0.3 of time)
- Increase between 0.01C - 0.09C (24 of time)
- Increase of lt 0.01C (14 of time)
- No impact when wind direction outside of
90-degree azimuth ARCON96 window (62 of time) - RH Impact
- Largest hourly RH impact 0.7
- ANSI/ANS-3.11 (2005) and NRC Regulatory Guide
1.23 Revision 1 accuracy requirements - Air temperature 0.5 C
- RH 4
17Conclusions
- Temperature and moisture increases due to
presence of discharge ponds at 10-meter tower not
significant - Slight increases
- Much smaller than ANSI/ANS-3.11 accuracy standard
for each parameter - Have no meaningful effect on meteorological data
used to evaluate environmental impacts of nuclear
power plant - No effect of discharge pond on wind speed and
wind direction is expected