Hi,
Use the different type of boundary for sediment as described in the SISYPHE manual and it can solve this problem:
The following thirteen variables for each edge point are first read out of the boundary conditions file:
X1, X2, X3, X4, X5, X6, X7, LIEBOR, EBOR, X10, X11, N, K.
LIEBOR is an integer providing the type of boundary conditions along the edges :
= KENT (numerical value 5): bottom evolution imposed to EBOR value at a liquid boundary,
= KSORT (numerical value 4): free evolution at a liquid boundary,
= KLOG or KADH (numerical value 2 or 0) : solid boundary.
EBOR provides the values of sedimentary evolutions when they are imposed.
A fixed bottom depth is usually imposed at the boundaries with an inflow (EBOR = 0; LIEBOR = KENT),
whereas a free evolution is imposed at the boundaries with an outflow (LIEBOR = KSORT).
Kind regards,
Qilong