Pore orientation of granular materials during biaxial compression

被引:10
作者
Kang, Dong Hun [1 ]
Yun, Tae Sup [2 ]
Evans, T. Matthew [3 ]
机构
[1] Yonsei Univ, Sch Civil & Environm Engn, Seoul 120749, South Korea
[2] Yonsei Univ, Dept Civil & Environm Engn, Seoul 120749, South Korea
[3] Oregon State Univ, Sch Civil & Construct Engn, Corvallis, OR 97331 USA
基金
新加坡国家研究基金会; 美国国家科学基金会;
关键词
Pore orientation; Tessellation; Principal stress; Biaxial compression; Discrete element method; Particle clump; SOIL-PARTICLE; SHEAR BANDS; SHAPE; CONSOLIDATION;
D O I
10.1016/j.compgeo.2014.03.004
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
The local pore spaces in granular materials tend to be aligned parallel to the major principal stress direction upon particle mobilization. Manifestation of this response has been numerically validated in our previous studies with the aid of discrete element method modeling and image processing techniques during creep and shearing. We now extend the modeling of pore geometry, constructed with spherical particles, to assemblies of particle clumps. Two-dimensional simulations are performed for both loose and dense assemblies of spherical particles and particle clumps. Each particle packing is bound by rigid or flexible walls and subjected to biaxial compression and the particle mobilization effect on the evolution of pore orientation is explored. Randomly shaped pores surrounded by adjacent particles are geometrically quantified by Delaunay tessellation and fitted with ellipses. Results show that localization is apparent in dense assemblies, in particular for clumped particle packing, while loose assemblies exhibit diffusive failure. Small pores within well-defined shear bands tend to align either parallel to the direction of the shear band or perpendicular to the major principal stress. On the other hand, small pores within the blocks and large pores have a tendency to become elongate towards the major principal stress direction. This study reveals for the first time that pore orientation is dependent upon particle shape, pore size, and assembly conditions on the pore and global scales. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1 / 11
页数:11
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