The plastic anisotropy of reconstituted soft soils is described from the compression behaviour observed during radial loading paths in stress space. A unique relationship is established between the orientation of the yield surface and the corresponding normal compression line, which indicates that a stabilized fabric is maintained under continuous loading along radial stress paths. The equilibrium orientation angle of the plastic potential surface is obtained explicitly. A new rotational hardening law is proposed by considering the dependence of the evolution of anisotropic fabric with the current stress condition and plastic strain. An elastoplastic constitutive model for anisotropic soil is formulated within the framework of Critical Stat...
The paper summarises the main results of a research into the very small strain shear stiffness of a ...
Soft clays are normally consolidated or lightly overconsolidated soils where even small increases of...
Natural soft clay exhibits a considerable degree of anisotropy as a result of its past sedimentation...
The plastic anisotropy of reconstituted soft soils is described from the compression behaviour obser...
Experimental data on Lower Cromer Till (LCT), a sandy silty-clay, are re-evaluated enabling a study ...
A rate-independent anisotropic elastoplastic constitutive model for natural soft clays is proposed, ...
Fundamental features of soft soil behaviour such as anisotropy, inter-particle bonding and destructu...
Recent laboratory investigations indicate that the stress-strain-strength responses of loose sands a...
Induced anisotropy is known to play a major role in the undrained strength of clays, especially in c...
The aim of the paper is to extend the experimental validation of the S-CLAY1 model, which is a recen...
A relationship between elastic anisotropy, as typically observed in clayey soils subjected to shear ...
An existing platform model for inherently anisotropic sands is extended to account for deformations ...
In this paper a relationship between elastic anisotropy, as typically observed in clayey soils subj...
A plasticity constitutive framework for modeling inherently anisotropic sand behavior is presented w...
Abstract:An anisotropic plasticity model is proposed to describe the fabric effect on sand behavior ...
The paper summarises the main results of a research into the very small strain shear stiffness of a ...
Soft clays are normally consolidated or lightly overconsolidated soils where even small increases of...
Natural soft clay exhibits a considerable degree of anisotropy as a result of its past sedimentation...
The plastic anisotropy of reconstituted soft soils is described from the compression behaviour obser...
Experimental data on Lower Cromer Till (LCT), a sandy silty-clay, are re-evaluated enabling a study ...
A rate-independent anisotropic elastoplastic constitutive model for natural soft clays is proposed, ...
Fundamental features of soft soil behaviour such as anisotropy, inter-particle bonding and destructu...
Recent laboratory investigations indicate that the stress-strain-strength responses of loose sands a...
Induced anisotropy is known to play a major role in the undrained strength of clays, especially in c...
The aim of the paper is to extend the experimental validation of the S-CLAY1 model, which is a recen...
A relationship between elastic anisotropy, as typically observed in clayey soils subjected to shear ...
An existing platform model for inherently anisotropic sands is extended to account for deformations ...
In this paper a relationship between elastic anisotropy, as typically observed in clayey soils subj...
A plasticity constitutive framework for modeling inherently anisotropic sand behavior is presented w...
Abstract:An anisotropic plasticity model is proposed to describe the fabric effect on sand behavior ...
The paper summarises the main results of a research into the very small strain shear stiffness of a ...
Soft clays are normally consolidated or lightly overconsolidated soils where even small increases of...
Natural soft clay exhibits a considerable degree of anisotropy as a result of its past sedimentation...