DEM investigation on the evolution of microstructure in granular soils under shearing

被引:185
作者
Gu, Xiaoqiang [1 ,2 ]
Huang, Maosong [1 ,2 ]
Qian, Jiangu [1 ,2 ]
机构
[1] Tongji Univ, Dept Geotech Engn, Shanghai 200092, Peoples R China
[2] Tongji Univ, Key Lab Geotechn & Underground Engn, Minist Educ, Shanghai 200092, Peoples R China
基金
中国国家自然科学基金;
关键词
Discrete element; Granular soil; Shear behavior; Microstructure; Anisotropy; Critical state; CRITICAL-STATE; INDUCED ANISOTROPY; STEADY-STATE; LIQUEFACTION; BEHAVIOR; SIMULATIONS; MODEL; DEFORMATION; SAND;
D O I
10.1007/s10035-013-0467-z
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The mechanical behaviors of granular soils at different initial densities and confining pressures in the drained and undrained triaxial tests are investigated micromechanically by three-dimensional discrete element method (DEM). The evolutions of the microstructure in the numerical specimen, including coordination number, contact force and anisotropies of contact normal and contact force, are monitored during the shearing. The typical shear behaviors of granular soils (e.g. strain softening, phase transformation, static liquefaction and critical state behavior) are successfully captured in the DEM simulation. It is found that the anisotropies of contact normal, normal and tangential contact forces comprise the shear resistance and show different evolution features during shearing. After large strain shearing, the microstructure of the soil will finally reach a critical state, although the evolution path depends on the soil density and loading mode. Similar to the macroscopic void ratio and deviatoric stress , the coordination number and anisotropies of contact normal and contact force at the critical state also depend on the mean normal effective stress at the critical state.
引用
收藏
页码:91 / 106
页数:16
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