Hello Professor Coulthard,
I have a fairly strong memory of reading a statement that CAESAR-Lisflood is not appropriate for cohesive soils, but I can't find that statement again. Perhaps it has been removed from an update? Or, not unlikely, I'm mistaken.
I see the lateral erosion rate is adjustable to affect the form of channels with narrow channels in a cohesive soil, but how does this interact with the grain size distribution? If clay-sized particles are mobilized based on the shear stress required to move them if not cohering to the bed wouldn't this still over predict incision?
I've experimented with piecewise planar profiles simulating a low-gradient clayey top slope leading to a steep bedrock side slope using grain size distributions determined by lab analyses and the top slope is ripped apart very quickly compared to what is seen in the field.
I'd appreciate your consideration and suggestions.
Cheers,
Kelly Crowell