Deformation of Granular Material under Continuous Rotation of Stress Principal Axes

被引:25
|
作者
Wang, Rui [1 ]
Fu, Pengcheng [2 ]
Zhang, Jian-Min [3 ]
Dafalias, Yannis F. [4 ,5 ]
机构
[1] Tsinghua Univ, Dept Hydraul Engn, State Key Lab Hydrosci & Engn, Beijing 100084, Peoples R China
[2] Lawrence Livermore Natl Lab, Atmospher Earth & Energy Div, 7000 East Ave, Livermore, CA 94551 USA
[3] Tsinghua Univ, Natl Engn Lab Green & Safe Construct Technol Urba, Beijing 100084, Peoples R China
[4] Univ Calif Davis, Dept Civil & Environm Engn, Davis, CA 95616 USA
[5] Natl Tech Univ Athens, Sch Appl Math & Phys Sci, Dept Mech, Athens 15780, Greece
基金
欧洲研究理事会; 中国国家自然科学基金;
关键词
Granular material; Continuous stress principal axes rotation; Discrete-element method; Deformation; Fabric; DISCRETE ELEMENT; SHEAR DEFORMATION; BEHAVIOR; ANISOTROPY; MODEL; SAND; STRENGTH; STRAIN; DEM;
D O I
10.1061/(ASCE)GM.1943-5622.0001383
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The mechanical response of granular material to the rotation of stress principal axes is an issue of both practical and theoretical importance in soilmechanics. This study used a two-dimensional (2D) discrete-element method (DEM) simulation to investigate the deformation of granular material under the continuous rotation of stress principal axes while maintaining fixed principal stress values. The results show that under such rotation, the deformation can exceed that caused by fixed principal stress axes cyclic biaxial compression with a maximum deviatoric stress ratio that equals the fixed stress ratio during rotation. The volumetric strain was found to be contractive overall while oscillating within each load cycle for specimens with significant fabric anisotropy. The initial fabric-anisotropy orientation was found to have little influence on the overall evolution of volumetric strain, although it was found to affect the development of shear strain. During the cycles of rotation of initial stress principal axes, the dilatancy of granular material, in the contractive direction, was found to be dominated by the evolving orientation of the major principal stress axis in reference to the initial major principal stress axis during anisotropic consolidation, and the influence of the initial fabric-anisotropy orientation was found to be trivial. As stress rotation continued, the influence of the relative orientation between stress and fabric became prominent, causing the material to dilate when the major principal stress axis rotated from the normal of the bedding plane to being perpendicular to it and causing contraction during the other half of the cycle. (c) 2019 American Society of Civil Engineers.
引用
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页数:15
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