“…The constitutive model used within the numerical code was the one named "Mohr-Coulomb" [32] for drained conditions, but the parameters were chosen to reproduce a rigid-plastic Tresca behavior in undrained conditions, i.e., the friction and dilatation angles were set equal to 0, the cohesion as c u , and E and ν were chosen as explained above. The Tresca criterion is the common one to reproduce the undrained shear strength of clays, but more complex soil constitutive laws that could more realistically reproduce, for example, soil displacements (e.g., [30]), and linearly increasing strength with depth (e.g., [11,17,18]) or clay strength anisotropy, are beyond the scope of the paper.…”