Modelling of time-varying dispersion for releases including ... - ukelg
Modelling of time-varying dispersion for releases including ... - ukelg
Modelling of time-varying dispersion for releases including ... - ukelg
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
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