ADDAM and CSA-ERM Modelling ADDAM and CSA-ERM Modelling Approach - - PowerPoint PPT Presentation

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ADDAM and CSA-ERM Modelling ADDAM and CSA-ERM Modelling Approach - - PowerPoint PPT Presentation

ADDAM and CSA-ERM Modelling ADDAM and CSA-ERM Modelling Approach and Results for the Approach and Results for the Mid-Range Scenario Mid-Range Scenario Presentation for IAEA Environmental Modelling for Radiation Safety (EMRAS-II), Urban Areas


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Sohan Chouhan Atomic Energy of Canada Limited Chalk River, Ontario, Canada ChouhanS@aecl.ca 2011 January 27

ADDAM and CSA-ERM Modelling Approach and Results for the Mid-Range Scenario ADDAM and CSA-ERM Modelling Approach and Results for the Mid-Range Scenario

Presentation for IAEA Environmental Modelling for Radiation Safety (EMRAS-II), Urban Areas Working Group Meeting, Vienna

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Features & Capabilities of ADDAM & CSA-ERM codes, and their comparison

  • Features and capabilities were introduced to this Working Group

(WG) in January 2010

  • Comparison was shown to this WG on Jan 25, 2011, the results

were produced by CSA-ERM, some were verified with ADDAM

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Application of the model to the mid-range scenario

  • CSA-ERM cannot handle spatial wind vectors, those were

summed outside the code

  • It has options for making either conservative or realistic

predictions; realistic options and parameter values were used in these calculations

  • The threshold wind speed for switching from the “short term

model” (where prediction can be made at any X and Y location) to the “prolonged term model” (where prediction can only be made

  • n the plume centerline sector and concentrations in all other

sectors become zero) was lowered from 2 m/s to 0 m/s.

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Adapting the data in the scenario description to the model

  • Cs-137 halflife ~ 30.17 years; I-131 halflife ~ 8.04 days
  • Cs-137 => Ba-137m (daughter reaches equilibrium with parent),

not considered

  • I-131 => Xe-131m (daughter never build close to parent), not

considered

  • Cs-137: 6.43e11 Bq released in one hour
  • I-131: 3.69e12 Bq released in one hour
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Assumptions made to match the model to the scenario

  • Air temperature: 20 Degree
  • No rain, no fog
  • Wind speed: 1.78 m/s for Stable; and 3.16 m/s for Neutral

situations

  • Stability class: E for stable conditions; and D for neutral conditions
  • Dry deposition velocity: best estimate; 0.01 m/s for Cs-137; 0.008

m/s for I-131; for grass surface

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Specific parameter values used for the scenario

  • Effective release height: 50 m; stack; downwash, plume rise, entrainment

and building wake effect not applied

  • Σy and Σz from stability class; short term dilution factor model used
  • Building constant Cb: 1
  • Inversion layer height: 1000 m for Stable; 1500 m for Neutral situations
  • Terrain cover: grass; roughness length: 0.4 m
  • Receptor height: 0 m
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Results: Deposited activity on the ground at the end of the simulation for Cs-137 release during stable met conditions

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Results (continued): Deposited activity on the ground for I-131 release during stable met conditions

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Results (continued): Deposited activity on the ground for Cs-137 release during neutral met conditions

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Results (continued): Deposited activity on the ground for I-131 release during neutral met conditions

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Results (continued): Time integrated air activity concentration at ground level for Cs-137 release during stable met conditions

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Results (continued): Time integrated air activity concentration at ground level for I-131 release during stable met conditions

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Results (continued): Time integrated air activity concentration at ground level for Cs-137 release during neutral met conditions

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Results (continued): Time integrated air activity concentration at ground level for I-131 release during neutral met conditions

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Results (continued): Time Series of activity concentration in air for release during stable met conditions

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Results (continued): Time Series of activity concentration in air for release during neutral met conditions

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Results (continued)

  • More detailed results were provided to the WG leader for

comparison

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Acknow ledgments to current ADDAM development and meteorological data collection team:

  • N. Scheier

The help from D. Killey in creating the plume contours is also much appreciated.

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