The various stress change with rotating principal axes act on soil in actual ground. The distribution of the interparticle contact normals, meanwhile, gradually tends to concentrate towards the direction of the major principal stress
σ1 when that of anisotropic stress acts on soil skeleton. And then, the stiffness of soil in the direction of major principal stress relatively increases. In ordinary model, such an induced anisotropy is considered by applying kinematic / rotational hardening rule in ordinary stress space. On the other hand, a new method, in which the induced anisotropy of soil is described simple and general isotropic hardening model by applying the modified stress which reflects the fabric change due to the variations of the intermediate principal stress and the stress histories, is developed in this study. The validity of the proposed model is verified by comparison with the experimental results of true triaxial tests on medium dense sand. It is shown that the proposed model, which obeys isotropic hardening rule and follows associated flow rule in
tij* space, suitably considers the influence of the intermediate principal stress and the past stress history simultaneously and properly reproduces the test results under various complicated three-dimensional stress path.
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