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Modelling of time-varying dispersion for releases including ... - ukelg

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UDM AWD <strong>dispersion</strong> <strong>including</strong> rainout UKELG 2013<br />

New observer method <strong>for</strong> <strong>time</strong>-<strong>varying</strong> release<br />

steady-state concentration curve <strong>for</strong> observer 1<br />

flow rate (kg/s)<br />

1<br />

2 3<br />

4<br />

5<br />

6<br />

Concentration<br />

3<br />

2<br />

1<br />

Concentration<br />

after along-wind diffusion<br />

Observer concentration<br />

(be<strong>for</strong>e along-wind diffusion)<br />

<strong>time</strong> (s)<br />

Time 1<br />

Release observers at regular <strong>time</strong> intervals<br />

6<br />

5<br />

4<br />

3<br />

Time 2<br />

2<br />

1<br />

Distance<br />

Carry out steady-state calculations <strong>for</strong> each observer<br />

At each output <strong>time</strong> set observer concentrations [be<strong>for</strong>e along-wind-diffusion]<br />

Apply along-wind diffusion and downwind spreading<br />

© Det Norske Veritas AS. All rights reserved.<br />

UDM along-wind diffusion <strong>for</strong>mulation<br />

(elevated finite-duration or <strong>time</strong>-<strong>varying</strong> release with no rainout, or <strong>dispersion</strong> from pool)<br />

“Observers” are released from source moving with UDM speed<br />

Algorithm to set concentration as function <strong>of</strong> position x and <strong>time</strong> t<br />

- Carry out Phast <strong>time</strong>-<strong>varying</strong> source-term calculations (flow rate or pool evaporation rate)<br />

- Divide in equal-mass segments<br />

- Calculations <strong>for</strong> each observer<br />

- Release observer at start <strong>of</strong> segment<br />

- Set <strong>time</strong>-<strong>varying</strong> observer data (downwind position ξ, concentration C o (ξ), …) from steady-state UDM run<br />

- At given <strong>time</strong> t , apply along-wind-diffusion by Gaussian integration over observer<br />

concentrations:<br />

Assumptions<br />

( x − ξ )<br />

∞<br />

2<br />

C<br />

c ( o<br />

( ξ ) ⎪⎧<br />

⎪⎫<br />

o<br />

x,<br />

t)<br />

= ∫<br />

exp ⎨−<br />

⎬dξ<br />

1/ 2<br />

0 ( 2π<br />

) σ<br />

x<br />

( ξ ) ⎪⎩ 2σ<br />

2<br />

x<br />

( ξ ) ⎪⎭<br />

- Ignore along-wind gravity spreading (no gravity shape correction)<br />

- No automation <strong>of</strong> observers and output <strong>time</strong>s<br />

- Use along-wind-diffusion coefficient σ x consistent with FDC method<br />

© Det Norske Veritas AS. All rights reserved. 15<br />

6

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