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ERDC TN-DOER-E10
April 2000
b. For the other size classes, SSFATE uses
Pi = 0, if τ ≥ τuli
(18)
Pi = 1.0, if τ ≤ τlli
(19)
where
τuli
= the shear stress above which no deposition occurs for grain class i
τlli
= the shear stress below which the deposition probability for grain class i is 1.0
Typical values for τRR, and τuR are given in
Table 2
Table 2.
Typical values for shear stresses, Pa
τlli
τuli
Class
A typical value for τcd is 0.016 Pa.
0
0.016
0.03
1
0.03
0.06
Next, the deposition of sediment from each size
2
0.06
0.20
class from each bottom cell during the current
3
0.20
0.90
time-step is computed. The computations start
with the largest size class:
Fluxi = bi Ci Wsi Pi
(20)
where bi is a probability parameter that includes all other factors influencing deposition other than
shear.
This mass is then removed from the particles occupying the cell. The deposition for the remaining
size classes is then computed, starting with the second largest size class and working down to the
smallest. This deposition is computed as follows:
If 0 ≤ Pi ≤ 0.05, then
C Fluxi +1
(21)
Ci +1 + 1
otherwise,
Fluxi = bi Ci Wsi Pi
(22)
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