Numerical simulation of macro-meso mechanical behaviours of sandstone containing a single open fissure under uniaxial compression

被引:12
作者
Wang, Bin [1 ,2 ]
Yao, Chi [1 ]
Yang, Jianhua [1 ]
Jiang, Shuihua [1 ]
机构
[1] Nanchang Univ, Sch Civil Engn & Architecture, Nanchang, Jiangxi, Peoples R China
[2] Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn, Wuhan, Hubei, Peoples R China
基金
中国国家自然科学基金;
关键词
Fissured rock; crack propagation; anisotropy; RBSM; 2 UNPARALLEL FISSURES; BLOCK SPRING METHOD; ROCK-LIKE MATERIAL; FRACTURE COALESCENCE; CRACK COALESCENCE; FAILURE; DAMAGE; FLAW;
D O I
10.1080/19648189.2017.1381647
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
By employing the improved rigid block spring method, the failure process of a sandstone example containing a single open fissure under uniaxial compression is modelled. In this method, the intact rock is considered as an assemblage of rigid polygonal blocks. Macro mechanical behaviours are governed by mechanical properties of interfaces between two neighbouring blocks. In the local scale on interfaces, both tensile splitting failure and shearing sliding failure are considered. Micro properties are obtained by a calibration procedure against the stress-strain curve of intact rock under uniaxial compression in the lab. Influences of fissure inclination and length on the uniaxial compression strength (UCS) and failure modes are discussed. Comparisons between numerical simulations and laboratory tests are presented. The growth process of micro-cracks is studied and the mechanism of micro-crack propagation is studied through analysis on the displacement evolution. Some conclusions are drawn: numerical results generally agree well with those from lab tests; the UCS of fissured rock is lower than the intact one; the UCS first goes down then goes up as inclination increases, but decreases gradually as fissure length increases; the micro failure modes are governed mainly by tensile splitting failures.
引用
收藏
页码:s99 / s113
页数:15
相关论文
共 24 条
[1]   Fracture coalescence in rock-type materials under uniaxial and biaxial compression [J].
Bobet, A ;
Einstein, HH .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 1998, 35 (07) :863-888
[2]   Deformability characteristics of jointed rock masses under uniaxial compression [J].
Xin, Chen ;
Liao Zhihong ;
Xi, Peng .
INTERNATIONAL JOURNAL OF MINING SCIENCE AND TECHNOLOGY, 2012, 22 (02) :213-221
[3]   Cracking process of rock mass models under uniaxial compression [J].
Chen Xin ;
Liao Zhi-hong ;
Peng Xi .
JOURNAL OF CENTRAL SOUTH UNIVERSITY, 2013, 20 (06) :1661-1678
[4]  
Fortune S., 1986, Proc. Second Ann. Symp. Comput. Geom. SCG New York, V86, P313
[5]  
Goodman R., 1968, J. Soil Mech. Found. Div., V94, P637, DOI 10.1061/JSFEAQ.0001133
[6]  
[郭彦双 GUO Yanshuang], 2007, [岩石力学与工程学报, Chinese Journal of Rock Mechanics and Engineering], V26, P525
[7]   Three-Dimensional Numerical Simulation on Triaxial Failure Mechanical Behavior of Rock-Like Specimen Containing Two Unparallel Fissures [J].
Huang, Yan-Hua ;
Yang, Sheng-Qi ;
Zhao, Jian .
ROCK MECHANICS AND ROCK ENGINEERING, 2016, 49 (12) :4711-4729
[8]  
Hudson J.A., 2000, ENG ROCK MECH INTRO
[9]   MICROCRACKS IN ROCKS - A REVIEW [J].
KRANZ, RL .
TECTONOPHYSICS, 1983, 100 (1-3) :449-480
[10]   Coalescence of multiple flaws in a rock-model material in uniaxial compression [J].
Sagong, M ;
Bobet, A .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 2002, 39 (02) :229-241