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An Analytical Screening Technique to Estimate the Effect of Cooling Ponds on Meteorological Measurements

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An Analytical Screening Technique to Estimate the Effect of Cooling Ponds on Meteorological Measurements A Case Study Stephen A. Vigeant, CCM and Carl A. Mazzola ... – PowerPoint PPT presentation

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Title: An Analytical Screening Technique to Estimate the Effect of Cooling Ponds on Meteorological Measurements


1
An 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
2
Outline
  • Introduction
  • Study Objective
  • Technical Approach
  • Sensible heat and moisture flux source terms
  • Atmospheric transport and diffusion
  • Results
  • Conclusions

3
Introduction
  • 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

4
Study 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

5
Technical 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

6
Sensible Heat and Moisture Fluxes
Wind
Sensible Heat Moisture Fluxes
Ta
Discharge Pond Ts
7
Technical 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)

8
Technical 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)

9
Technical 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)

10
Technical 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)

11
Technical 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

12
Technical 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

13
Technical 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

14
Technical 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

15
Technical 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)

16
Results
  • 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

17
Conclusions
  • 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
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