Constitutive modeling of principal stress rotation by considering inherent and induced anisotropy of soils

被引:53
作者
Tian, Yu [1 ]
Yao, Yang-Ping [1 ]
机构
[1] Beihang Univ, Sch Transportat Sci & Engn, Beijing 100083, Peoples R China
基金
中国国家自然科学基金;
关键词
Anisotropy; Constitutive model; Fabric; Principal stress rotation; Soil; Transformed stress; CRITICAL-STATE THEORY; UH MODEL; UNDRAINED ANISOTROPY; SAND; BEHAVIOR; DEFORMATION; SHEAR; CLAY;
D O I
10.1007/s11440-018-0680-3
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In order to simulate the soil response during principal stress rotation, anisotropic unified hardening (UH) model is developed within the framework of elastoplastic theory. Without introducing any additional mechanism to display the role of stress rotation specifically, this model achieves the simulation by considering the material anisotropy. The effect of inherent anisotropy is reflected using the anisotropic transformed stress method, but a new formula for the stress mapping is adopted to keep the mean stress unchanged. Analysis indicates that from the view of the transformed stress tensor, the anisotropic soil is subjected to loading during pure rotation of principal stress axes, so that plastic strains can be calculated. To represent the induced anisotropy, a fabric evolution law is proposed based on laboratory and numerical test results. At the critical state, the fabric tensor reaches a stable value determined by the stress state, while the critical state line is unique in the plane of void ratio versus mean stress. The anisotropic UH model has concise formulation and explicit elastoplastic flexibility matrix and can provide reasonable predictions for the deformation of anisotropic soils when principal stresses rotate.
引用
收藏
页码:1299 / 1311
页数:13
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