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X/Q for Releases From Area Sources 2009 RETS-REMP Workshop Jim Key Key Solutions, Inc. www.keysolutionsinc.com
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Concerns Industry Tritium Issues Have Revealed Many Unanalyzed Dose Pathways –Storm Drains –Ground Water –Service Water –Discharge Basins or Lakes With Little Water Turnover
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Evaporation From Area Sources Has Been Mostly Ignored Tritium Concentrations in Bodies of Water Can Continue to Build Up Release from Such Sources are Estimated to be 10 Ci/yr and Higher
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Application of Gaussian Model to Release from Area Sources Simplify Gaussian Model As Follows –Ground Level Release –Ground Level Receptor Modify From Point Source Geometry to Square Area Geometry
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Examine Point Source Plume Centerline Point Source Sector Average Area Source Plume Centerline Area Source Sector Average
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Standard Gaussian Model
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General Gaussian X/Q Downwind Factor Crosswind Factor Vertical Factor
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General Gaussian X/Q
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Horizontal and Vertical Parameters y (x) and z (x) are functions of –Downwind Distance – x –Atmospheric Stability – Pasquill Category
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y Lateral Diffusion Coefficients
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z Vertical Diffusion Coefficients
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Atmospheric Stability Categories Stability CategoryConditionDescription Lapse Rate AExtremely UnstableSunny Summer Weather-1.9 BModerately StableSunny and Warm-1.9 to –1.7 CSlightly UnstableAverage Day-1.7 to –1.5 DNeutralOvercast Day or Night-1.5 to –0.5 ESlightly StableAverage Night-0.5 to 1.5 FModerately StableClear Night1.5 to 4.0 GHighly StableAdded by NRC> 4.0
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Simplifications Ground Level Release –Set H = 0 Ground Level Receptor –Set z = 0 Plume Centerline –Set y = 0
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Ground Level Concentration Ground Level Receptor Plume Centerline Point Source
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Point Source Geometry Receptor Wind Point Source x
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Sector Averaged Concentration Wind Directions in Each Sector are Distributed Randomly Over Period of Interest Calculate Average Value of /Q for Sector Length
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Calculate Average Value of Function Over Sector Length
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Find Average Value of /Q over Sector Arc Length
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Crosswind Integrated Concentration This term is cannot be integrated analytically
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Easier to Use… From Standard Math Tables
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Crosswind Integrated Concentration Function Of Only –Downwind Distance – x –Wind Speed - u
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Ground Level Concentration Ground Level Receptor Sector Average Point Source
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Time-Averaged Concentration Wind Directions in Each Sector are Distributed Randomly Over Period of Interest Calculate X/Q Using Joint Frequency Distribution: f( ,S,N) – Direction –SStability Class –NWind Speed Class
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Time-Averaged Concentration Allowed By NRC Guidance –Reg Guides 1.109 –NUREGs 0133, 0472, 0473, 1301, 1302 Less Scatter and Variability Than Real Data Dose Models Are Based On 1 Year Annual Exposure
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/Q Variability Real Time/Short Term /Q –Factors of 3 to 10 Long Term /Q –Factors of 2 to 4 From NCRP Report No. 76
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Applying JFD Data to X/Q Use Average Wind Speed (Not Max Wind Speed) Determine yo for Each Stability Class Determine Virtual Distance (X v ) for Each Stability Class
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Calculate X/Q Using:
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Now Consider Area Source Simplifications –Ground Level Release –Ground Level Receptor Assume Point Source at Center of Release –Very Conservative –Does not consider that source is initially distributed over large surface area. Plume Centerline Sector Average
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Area Source For Plume Centerline Assumes Ground Level Release Ground Level Receptor Simple Geometry
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Simple Geometry for Near Field Area Source Wind Area Source Receptor 2b 2a
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Calculate Average Value of Function Over An Area Integration Over Area of Source Calculates Plume Centerline Concentration
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Ground Level Concentration Near field conditions or large area sources require that we consider y (x) and z (x) as functions of x
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Problem to Solve
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Problem to Solve - 2 Cannot Be Solved Analytically Use Error Function for Integral Over dy
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Error Function Erf
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Error Function Identities
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Problem to Solve - 3 Replace With
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Problem to Solve - 4
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Problem to Solve - 5 Reduced to Integral of dx Integrate Using Simpson’s Rule
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Area Source For Sector Average Similar Development for Point Source Results In - Cannot Be Integrated Analytically Integrate Using Simpson’s Rule –Simpler Function to Integrate Numerically
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Simple Case Calculate X/Q Assuming –Ground Level Release –Emission Source is One Mile Square –Receptor is Due West ½ Mile from Center of Source (i.e. at Boundary) –Assume Worst Case Met Conditions Extremely Stabile (Class G) Calm Conditions (0.04 m/s) Least Dispersion
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Example 1 Ground Level Release Emission Source is One Mile Square Receptor is Due West ½ Mile from Center of Source (i.e. at Area Boundary) Assume Worst Case Met Conditions –Extremely Stabile (Class G) –Calm Conditions (0.04 m/s) –Least Dispersion
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Point Source vs Area Source Receptor Wind Point Source 1600 meters Area Source
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Example 1 Calculations Geometry /Q (m/sec2) Point Source Plume Centerline 9.2E-02 Point Source Sector Average 1.5E-02 Area Source Plume Centerline 6.6E-03 Area Source Sector Average 3.2E-03 Source = 1 Square Mile Receptor at Source Boundary
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Simple X/Q for Area Source u = 0.022 m/s x = 20,800 m zG = 7.5 m
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Geometry for Example 2 1600 meters Receptor Point Source Wind 3200 meters
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Example 2 Calculations Geometry /Q (m/sec2) Point Source Plume Centerline 8.1E-03 Point Source Sector Average 1.2E-03 Area Source Plume Centerline 9.2E-06 Area Source Sector Average 5.7E-04 Source = 1 Square Mile Receptor 2 Miles From Boundary
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Point Source vs Area Source X/Q Larger Sources – Expect Greater Difference As Distance to Receptor Increases Difference Slowly Decreases
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ALOHA
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