Modeling Micro-cracking Behavior of Bukit Timah Granite Using Grain-Based Model

被引:147
作者
Peng, Jun [1 ,2 ,3 ]
Wong, Louis Ngai Yuen [2 ]
Teh, Cee Ing [3 ]
Li, Zhihuan [3 ]
机构
[1] Wuhan Univ, State Key Lab Water Resources & Hydropower Engn S, Wuhan, Hubei, Peoples R China
[2] Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China
[3] Nanyang Technol Univ, Sch Civil & Environm Engn, Singapore, Singapore
基金
中国博士后科学基金; 中国国家自然科学基金;
关键词
Grain-based model; Grain boundary cracks; Intra-grain cracks; Micro-cracking behavior; Failure mode; BONDED-PARTICLE MODEL; ROCK-LIKE MATERIAL; UNIAXIAL COMPRESSION; TRIAXIAL COMPRESSION; WESTERLY GRANITE; BRITTLE ROCK; ACOUSTIC-EMISSION; ENERGY-DISSIPATION; CRACKING PROCESSES; CRYSTALLINE ROCKS;
D O I
10.1007/s00603-017-1316-x
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Rock strength and deformation behavior has long been recognized to be closely related to the microstructure and the associated micro-cracking process. A good understanding of crack initiation and coalescence mechanisms will thus allow us to account for the variation of rock strength and deformation properties from a microscopic view. This paper numerically investigates the micro-cracking behavior of Bukit Timah granite by using a grain-based modeling approach. First, the principles of grain-based model adopted in the two-dimensional Particle Flow Code and the numerical model generation procedure are reviewed. The micro-parameters of the numerical model are then calibrated to match the macro-properties of the rock obtained from tension and compression tests in the laboratory. The simulated rock properties are in good agreement with the laboratory test results with the errors less than +/- 6%. Finally, the calibrated model is used to study the micro-cracking behavior and the failure modes of the rock under direct tension and under compression with different confining pressures. The results reveal that when the numerical model is loaded in direct tension, only grain boundary tensile cracks are generated, and the simulated macroscopic fracture agrees well with the results obtained in laboratory tests. When the model is loaded in compression, the ratio of grain boundary tensile cracks to grain boundary shear cracks decreases with the increase in confining pressure. In other words, the results show that as the confining pressure increases, the failure mechanism changes from tension to shear. The simulated failure mode of the model changes from splitting to shear as the applied confining pressure gradually increases, which is comparable with that observed in laboratory tests. The grain-based model used in this study thus appears promising for further investigation of microscopic and macroscopic behavior of crystalline rocks under different loading conditions.
引用
收藏
页码:135 / 154
页数:20
相关论文
共 82 条
[1]   Characterisation of microcracks in the Bohus granite, western Sweden, caused by uniaxial cyclic loading [J].
Åkesson, U ;
Hansson, J ;
Stigh, J .
ENGINEERING GEOLOGY, 2004, 72 (1-2) :131-142
[2]  
[Anonymous], 1971, PROC S INT SOC ROCK
[3]  
[Anonymous], 1994, B INT ASS ENG GEOLOG, DOI DOI 10.1007/BF02595006
[4]  
[Anonymous], 2008, PART FLOW COD 2 DIM
[5]  
Bahrani N., 2012, 21st Canadian rock mechanics symposium: RockEng12-Rock Engineering for Natural Resources, Edmonton: Canada, P485
[6]   Numerical investigation of the influence of specimen size on the unconfined strength of defected rocks [J].
Bahrani, Navid ;
Kaiser, Peter K. .
COMPUTERS AND GEOTECHNICS, 2016, 77 :56-67
[7]   Distinct element method simulation of an analogue for a highly interlocked, non-persistently jointed rockmass [J].
Bahrani, Navid ;
Kaiser, Peter K. ;
Valley, Benoit .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 2014, 71 :117-130
[8]  
Bass JD., 1995, Mineral Physics and Crystallography, A handbook of Physical Constants, DOI DOI 10.1029/RF002P0045
[9]   MICROCRACK CLOSURE IN ROCKS UNDER STRESS - DIRECT OBSERVATION [J].
BATZLE, ML ;
SIMMONS, G ;
SIEGFRIED, RW .
JOURNAL OF GEOPHYSICAL RESEARCH, 1980, 85 (NB12) :7072-7090
[10]   DEM Simulation of Direct Shear: 2. Grain Boundary and Mineral Grain Strength Component Influence on Shear Rupture [J].
Bewick, R. P. ;
Kaiser, P. K. ;
Bawden, W. F. .
ROCK MECHANICS AND ROCK ENGINEERING, 2014, 47 (05) :1673-1692