Modeling the entire progressive failure process of rock slopes using a strength-based criterion

被引:128
|
作者
Yang, Yongtao [1 ]
Xu, Dongdong [2 ]
Liu, Feng [3 ]
Zheng, Hong [1 ,4 ]
机构
[1] Chinese Acad Sci, State Key Lab Geomech & Geotech Engn, Inst Rock & Soil Mech, Wuhan 430071, Peoples R China
[2] Changjiang River Sci Res Inst, Key Lab Geotech Mech & Engn, Minist Water Resources, Wuhan 430010, Peoples R China
[3] Tianjin Univ, State Key Lab Hydraul Engn Simulat & Safety, Sch Civil Engn, Tianjin 300072, Peoples R China
[4] Beijing Univ Technol, Key Lab Urban Secur & Disaster Engn, Minist Educ, Beijing 100124, Peoples R China
基金
中国国家自然科学基金;
关键词
Crack propagation; Rock slope; Progressive failure; Numerical manifold method; NUMERICAL MANIFOLD METHOD; UNCONFINED SEEPAGE FLOW; CRACK-PROPAGATION; FRACTURE PROPAGATION; STABILITY ANALYSIS; RESPONSE ANALYSIS; MESHFREE METHOD; POROUS-MEDIA; DEFORMATION; SIMULATION;
D O I
10.1016/j.compgeo.2020.103726
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
To simulate the entire process of the progressive failure of rock slopes, a series of techniques are incorporated into the original NMM (numerical manifold method). To reflect the stress concentration near the crack tip, the Williams' displacement series is adopted to enrich the global displacement function of the NMM. Furthermore, the most recently proposed strength-based LT criterion, which can account for tensile cracks, tensile-shear cracks and compressive-shear cracks, is adopted to determine the crack propagation direction and length. Three typical numerical examples, including a Mode-I crack problem, a Mode-II crack problem and a Brazilian disc problem are adopted to verify the numerical model. The numerical results indicate that the numerical model is capable of accurately simulating the Mode-I crack propagation problem, the mode-II crack propagation problem and the failure process of Brazilian disc. Furthermore, the numerical model is adopted to investigate the entire progressive failure process of two rock slopes. The corresponding results indicate that the numerical model can not only simulate the propagation and coalescence of multiple cracks in rock masses but also the opening/sliding of rock blocks along discontinuities. The proposed numerical model warrants further investigation.
引用
收藏
页数:12
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