Cavitation Stress

Hi

I was modelling a deep excavation in clay (modeled as undrained B), and upon inspecting the results, I noticed the generation of high positive porewater pressure (pexcess is large and positive,  psteady is negative as it should be, and the resulting pactive is large and positive) at the bottom of excavation. To address this, I capped the pactive at the default Patmospheric, and the problem stopped converging after a certain depth of excavation. The same problem was converging when the cavitation cap was not applied. This was surprising especially when using undrained B, since the strength is independent on the effective stress (and hence the pwp) and the shear stress should be similarly independent on the pwp (total shear stress = effective shear stress).

I referred to the reference manual to check the way the cavitation cap is applied, and found no mentioning of how this cap is reflected back on stresses and the equilibrium of the problem. I also compared the TOTAL stresses with and without the cavitation cap, and they are certainly different which is also confusing.

I would appreciate some insight on this issue, because i am not sure now whether this "soil body seems to collapse" after i apply the cavitation cap is indicating a real basal stability problem or it is just an error or limitation in the implementation of this feature.

Thank you

(Software = Plaxis 3D; Soil Models: HS and HS small)