Research on failure modes in fractured rock masses under triaxial compression using Distinct Element Method

被引:0
作者
Fan, Lei [1 ]
Tang, Huiming [2 ]
Zhou, Huoming [1 ]
机构
[1] Yangtze River Sci Res Inst, Minist Water Resources, Key Lab Geotech Mech & Engn, Wuhan 430010, Peoples R China
[2] China Univ Geosci, Fac Engn, Wuhan 430074, Peoples R China
来源
INFORMATION TECHNOLOGY IN GEO-ENGINEERING | 2010年
关键词
Fractured rock mass; failure strength; failure modes; numercial test; Distinct Element Method; STRENGTH; BEHAVIOR;
D O I
10.3233/978-1-60750-617-1-686
中图分类号
TP [自动化技术、计算机技术];
学科分类号
0812 ;
摘要
Because of large number of discontinuities existing in rock mass, the mechanics and failure modes are controlled by the rock mass structure characteristics. The numerical test method, integrating the results of in-situ investigations, laboratory and in-site tests, can provide a new approach to study the mechanical behavior and failure theory of fractured rock mass. The fractured sandstone rock masses in the west area of Hubei Province were chosen as a case study. Based on the statistic analyses of discontinuities, the structure models of rock masses are founded with Monte-Carlo method. Then a series of numerical compress tests using Distinct Element Method were carried out to discuss the failure strengths and failure modes in rock masses. The study shows that, the failure strengths and failure modes have a strong dependency on model size, confining pressure and loading orientation. In addition, the fractured rock mass shows anisotropic behavior, but this behavior is insignificant with the increase of confining pressure and the side length of rectangle model. The failure modes in fractured rock masses can be generalized into two types. One occurs in a complex way in small models under high confining pressures, i. e., combining sliding and bursting of discontinuities and shear bands in the rock matrix. Another takes place with slide of discontinuities in small models under low confining pressures or in large models. However, the pathways of these two failure modes both have an angle of 30 degrees to 45 degrees to the loading orientation.
引用
收藏
页码:686 / 693
页数:8
相关论文
共 14 条
[1]   INTRINSIC SHEAR-STRENGTH OF A BRITTLE, ANISOTROPIC ROCK .3. TEXTURAL INTERPRETATION OF FAILURE [J].
ATTEWELL, PB ;
SANDFORD, MR .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 1974, 11 (11) :439-451
[2]   A modified single plane of weakness theory for the failure of highly stratified rocks [J].
Duveau, G ;
Shao, JF .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 1998, 35 (06) :807-813
[3]  
EINSTEIN HH, 1983, INT J ROCK MECH MIN, V20, P227, DOI 10.1016/0148-9062(83)90003-7
[4]  
Goodman R.E., 1976, Methods of Geological Engineering in Discontinuous Rocks
[5]   Practical estimates of rock mass strength [J].
Hoek, E ;
Brown, ET .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 1997, 34 (08) :1165-1186
[6]   Physical and particle flow modeling of jointed rock block behavior under uniaxial loading [J].
Kulatilake, PHSW ;
Malama, B ;
Wang, JL .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 2001, 38 (05) :641-657
[7]   Numerical determination of the equivalent elastic compliance tensor for fractured rock masses using the distinct element method [J].
Min, KB ;
Jing, LR .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 2003, 40 (06) :795-816
[8]   Anisotropic strength and deformational behavior of Himalayan schists [J].
Nasseri, MHB ;
Rao, KS ;
Ramamurthy, T .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 2003, 40 (01) :3-23
[9]  
Peter Attewell B., 1974, INT J ROCK MECH MIN, V11, P431
[10]  
Peter Attewell B., 1974, INT J ROCK MECH MIN, V11, P423