FDEM Simulation of Rocks with Microstructure Generated by Voronoi Grain-Based Model with Particle Growth

被引:44
作者
Zhou, Wei [1 ,2 ]
Ji, Xiang [1 ,2 ]
Ma, Gang [1 ,2 ]
Chen, Yuan [1 ,2 ]
机构
[1] Wuhan Univ, State Key Lab Water Resources & Hydropower Engn, Wuhan 430072, Hubei, Peoples R China
[2] Wuhan Univ, Minist Educ, Key Lab Rock Mech Hydraul Struct Engn, Wuhan 430072, Hubei, Peoples R China
基金
国家重点研发计划; 美国国家科学基金会;
关键词
Grain-based model; Particle growth; FDEM; Petrographic analysis; BUKIT TIMAH GRANITE; MICROCRACKING BEHAVIOR; STRENGTH; BRITTLE; STRESS; FAILURE; SIZE; FRAGMENTATION; IMPACT; ENERGY;
D O I
10.1007/s00603-019-02014-0
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Rock strength variation is closely related to its microstructure. With the development of computer technology, the numerical model of rocks can be constructed via computer programming, and the numerical simulation avoids a mass of redundant experimental tests and usually limited by the samples retrieved from the sub-surfaces. In previous studies, the microstructure in the numerical model is generated randomly. In this paper, a novel methodology for generating the polycrystalline rock microstructure by a Voronoi grain-based model with particle growth is proposed. The 3D Voronoi tessellations in this numerical model generation procedure do not consist of random poly-crystals; the distribution of the poly-crystals varies in shapes and sizes, which represent different mineral grains, and is determined by petrographic data with the 3D particle growth method. The uniaxial compression tests and tension tests are simulated via a combined FDEM and cohesive crack propagation model. The results demonstrate that the numerical simulation agrees well with the experimental study. More importantly, the fracture patterns in the micro-scale are gained, similar to the results obtained from laboratory experiments. The novel Voronoi grain-based model with the particle growth method can reconstruct the microstructure of polycrystalline rocks and provide further information in understanding the micro-behaviors of rock materials.
引用
收藏
页码:1909 / 1921
页数:13
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