TY - JOUR
T1 - Stress-strain model for clays with anisotropic void ratio distribution
AU - Masad, Eyad
AU - Muhunthan, Balasingam
AU - Chameau, Jean Lou
PY - 1998/5
Y1 - 1998/5
N2 - The porosity of soils is considered to be a directional measure and its distribution is characterized by a functional form. This form has been used to extend the critical state soil mechanics framework to include the effects of structure in soils. A new internal plastic energy dissipation formulation has been proposed to account for fabric arrangement. New expressions for the yield locus, and the plastic stress-strain response of structural soils have been derived. The applicability of the concepts to model the plastic stress-strain behaviour of a number of soils is illustrated. The advantage of the new model is very well indentified in modelling the stress-strain behaviour of K0 consolidated and natural clays.
AB - The porosity of soils is considered to be a directional measure and its distribution is characterized by a functional form. This form has been used to extend the critical state soil mechanics framework to include the effects of structure in soils. A new internal plastic energy dissipation formulation has been proposed to account for fabric arrangement. New expressions for the yield locus, and the plastic stress-strain response of structural soils have been derived. The applicability of the concepts to model the plastic stress-strain behaviour of a number of soils is illustrated. The advantage of the new model is very well indentified in modelling the stress-strain behaviour of K0 consolidated and natural clays.
UR - http://www.scopus.com/inward/record.url?scp=0032075873&partnerID=8YFLogxK
U2 - 10.1002/(SICI)1096-9853(199805)22:5<393::AID-NAG922>3.0.CO;2-W
DO - 10.1002/(SICI)1096-9853(199805)22:5<393::AID-NAG922>3.0.CO;2-W
M3 - Article
AN - SCOPUS:0032075873
SN - 0363-9061
VL - 22
SP - 393
EP - 416
JO - International Journal for Numerical and Analytical Methods in Geomechanics
JF - International Journal for Numerical and Analytical Methods in Geomechanics
IS - 5
ER -