Micro-mechanical analysis of one-dimensional compression of clay with DEM

被引:51
作者
Wang, Pei [1 ,2 ]
Yin, Zhen-Yu [2 ,5 ]
Hicher, Pierre-Yves [3 ]
Cui, Yu-Jun [4 ]
机构
[1] East China Jiaotong Univ, Sch Civil Engn & Architecture, Inst Geotech Engn, Nanchang, Jiangxi, Peoples R China
[2] Hong Kong Polytech Univ, Dept Civil & Environm Engn, Kowloon, Hong Kong, Peoples R China
[3] Ecole Cent Nantes, Res Inst Civil Engn & Mech GeM, UMR CNRS 6183, Nantes, France
[4] Ecole Ponts ParisTech, CERMES, Lab Navier, Paris, France
[5] Hong Kong Polytech Univ, Dept Civil & Environm Engn, Kowloon, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
clay; compressibility; contact law; discrete element method; micromechanics; microstructure; DISCRETE-ELEMENT METHOD; ELECTROLYTE CONCENTRATION; NUMERICAL-SIMULATION; DOUBLE-LAYER; BEHAVIOR; SOILS; THICKNESS; CHARGE; MODEL;
D O I
10.1002/nag.3597
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In order to clarify the micro-mechanics of clay during compression, the behavior of clay subjected to one-dimensional compression is investigated at the particle scale using discrete element method (DEM). The flaky clay particles in the simulation are approximated by clumps made of spheres. A new contact model is implemented to account for the double-layer repulsive force, the van der Waals attractive force and the mechanical contact force. The effect of sphere arrangement in the particle clump is discussed. The DEM model is validated against experimental observations in terms of macroscopic compressibility, particle dip angle as well as the over consolidated behavior. The e-log & sigma;(v) curve shows a concave-to-linear shape. The evolution of dip angle of clay particles indicates that particles tend to have an anisotropy with a preferential orientation towards horizontal direction. The increase of preconsolidation pressure decreases the initial compressibility due to the increase the number of mechanical contacts. The evolution of average coordination and sphere-sphere contact shows that the majority of mechanical contacts are generated before the compressive stress reaches 100 kPa. Evolution of soil fabric is presented and discussed.
引用
收藏
页码:2706 / 2724
页数:19
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