This paper reports about the derivation of a fully nonlinear model characte
rized by finite deformations without smallness assumptions. The soil is ass
umed to be saturated, and no restrictions are introduced on the constitutiv
e laws. Initial boundary value problems are formulated with reference to ge
otechnical problems, such as consolidation under own weight or sedimentatio
n of solid particles in a quiescent fluid, and back-analyses of field perfo
rmance of an embankment resting on a soft clay deposit.