Abstract
This paper presents a poro-visco-elastic-plastic damageable model for saturated frozen soils within a rigorous theoretical framework. The effective fluid pressure, obtained considering the interfacial energy, is combined with the total Cauchy stress in order to formulate the hydro-mechanical effective stress applied to a soil skeleton. On the other hand, a two-stress variable constitutive relationship is adopted for saturated frozen soils to describe the essential features of frozen and unfrozen behaviour. Based on the continuum damage theory, the cross-anisotropic damage variables for saturated frozen soils are deduced. The proposed damage criterion and the new nonlinear damage surface for saturated frozen soils are all governed by the second invariants of the “double effective stress”, which combines the damaged effective stress with the effective hydro-mechanical stress. The validity of the visco-elasto-plastic model with no damage is verified by comparing its modelling results with experimental results obtained from uniaxial creep tests.
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