In this paper, a noncoaxial plane strain soil model is developed in the framework of initial soil strength anisotropy that is described by taking the internal friction angle to be a function of principal stress orientations. The conventional Mohr-Coulomb (M-C) yield criterion is generalized to give an anisotropic yield criterion, with the curve in the deviatoric stress space forming an ellipse. Both rotational and eccentric ellipses are discussed. The formulation of noncoaxial constitutive equations is described by a general form in terms of the plastic strain rate. In this form, the plastic strain rate is divided into two parts: the conventional component that is derived from the classical plastic potential theory and the noncoaxial compon...
Nowadays, constitutive models for soils used for numerical modelling of tunnelling are normally rest...
The shear vane test is a method of determining the in-situ undrained strength and remolded shear str...
Natural soft clay exhibits a considerable degree of anisotropy as a result of its past sedimentation...
A novel, non-coaxial soil model is developed in the context of perfect plasticity for the plane stra...
The significant influence of transverse isotropy on mechanical behaviours of soil has long been reco...
Rotational shear is the type of loading path where samples are subjected to cyclic rotation of princ...
Fundamental features of soft soil behaviour such as anisotropy, inter-particle bonding and destructu...
Recent experimental investigations have highlighted the impact of principal stress rotation on soil ...
A major problem in soil mechanics is the prediction of stresses and displacements under loads applie...
In this paper, an anisotropic non-associative constitutive model, based on the well-established crit...
The non-coaxality of constitutive relationship has strongly influenced the predictions of the incept...
This paper presents an elastoplastic soil model considering the Principal Stress Rotation (PSR) and ...
Soil fabric and its evolving nature underpin the non-coaxial, anisotropic mechanical behaviour of sa...
Previous researches have indicated the non-coaxiality of sand in unidirectional simple shear tests, ...
This paper presents an experimental investigation revisiting the anisotropic stress–strain–strength ...
Nowadays, constitutive models for soils used for numerical modelling of tunnelling are normally rest...
The shear vane test is a method of determining the in-situ undrained strength and remolded shear str...
Natural soft clay exhibits a considerable degree of anisotropy as a result of its past sedimentation...
A novel, non-coaxial soil model is developed in the context of perfect plasticity for the plane stra...
The significant influence of transverse isotropy on mechanical behaviours of soil has long been reco...
Rotational shear is the type of loading path where samples are subjected to cyclic rotation of princ...
Fundamental features of soft soil behaviour such as anisotropy, inter-particle bonding and destructu...
Recent experimental investigations have highlighted the impact of principal stress rotation on soil ...
A major problem in soil mechanics is the prediction of stresses and displacements under loads applie...
In this paper, an anisotropic non-associative constitutive model, based on the well-established crit...
The non-coaxality of constitutive relationship has strongly influenced the predictions of the incept...
This paper presents an elastoplastic soil model considering the Principal Stress Rotation (PSR) and ...
Soil fabric and its evolving nature underpin the non-coaxial, anisotropic mechanical behaviour of sa...
Previous researches have indicated the non-coaxiality of sand in unidirectional simple shear tests, ...
This paper presents an experimental investigation revisiting the anisotropic stress–strain–strength ...
Nowadays, constitutive models for soils used for numerical modelling of tunnelling are normally rest...
The shear vane test is a method of determining the in-situ undrained strength and remolded shear str...
Natural soft clay exhibits a considerable degree of anisotropy as a result of its past sedimentation...