Calibration of coupled hydro-mechanical properties of grain-based model for simulating fracture process and associated pore pressure evolution in excavation damage zone around deep tunnels

被引:30
作者
Farahmand, Kiarash [1 ,2 ]
Diederichs, Mark S. [1 ]
机构
[1] Queens Univ, Dept Geol Sci & Geol Engn, Kingston, ON K7L 3N6, Canada
[2] Golder Associates, Vancouver, BC, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
Coupled hydro-mechanical properties; Excavation damage zone (EDZ); Grain-based model (GBM) calibration; Stress-fracturing of rock; Cohesive crack model; Stress-dependent permeability; CANADIAN GEOTECHNICAL COLLOQUIUM; PERMEABILITY CHANGES; CRACK-PROPAGATION; ROCK; FAILURE; STRESS; STRENGTH; MECHANISMS; URL; LAW;
D O I
10.1016/j.jrmge.2020.06.006
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The objective of this paper is to develop a methodology for calibration of a discrete element grain-based model (GBM) to replicate the hydro-mechanical properties of a brittle rock measured in the laboratory, and to apply the calibrated model to simulating the formation of excavation damage zone (EDZ) around underground excavations. Firstly, a new cohesive crack model is implemented into the universal distinct element code (UDEC) to control the fracturing behaviour of materials under various loading modes. Next, a methodology for calibration of the components of the UDEC-Voronoi model is discussed. The role of connectivity of induced microcracks on increasing the permeability of laboratory-scale samples is investigated. The calibrated samples are used to investigate the influence of pore fluid pressure on weakening the drained strength of the laboratory-scale rock. The validity of the Terzaghi's effective stress law for the drained peak strength of low-porosity rock is tested by performing a series of biaxial compression test simulations. Finally, the evolution of damage and pore pressure around two unsupported circular tunnels in crystalline granitic rock is studied. (C) 2021 Institute of Rock and Soil Mechanics, Chinese Academy of Sciences. Production and hosting by Elsevier B.V.
引用
收藏
页码:60 / 83
页数:24
相关论文
共 88 条
[1]  
ANDRA, 2005, EV FEAS GEOL REP ARG
[2]  
[Anonymous], 2007, The complete ISRM Suggested Mehtods for Rock Characterization, Testing, and Monitoring: 1974-2006
[3]  
[Anonymous], 2000, THESIS U WATERLOO WA
[4]  
ATKINSON C, 1982, INT J FRACTURE, V18, P279
[5]  
Backers T., 2005, FRACTURE TOUGHNESS D
[6]   FUNDAMENTALS OF ROCK JOINT DEFORMATION [J].
BANDIS, SC ;
LUMSDEN, AC ;
BARTON, NR .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 1983, 20 (06) :249-268
[7]  
Bass J.D., 1995, Mineral Phy. Crystallograph.: Handbook Phy. Constants, V2, P45, DOI [DOI 10.1029/RF002P0045, 10.1029/RF002p0045]
[8]  
Bear Jacob, 2013, Dynamics of fluids in porous media. New York
[9]   DEM Simulation of Direct Shear: 1. Rupture Under Constant Normal Stress Boundary Conditions [J].
Bewick, R. P. ;
Kaiser, P. K. ;
Bawden, W. F. ;
Bahrani, N. .
ROCK MECHANICS AND ROCK ENGINEERING, 2014, 47 (05) :1647-1671
[10]   General theory of three-dimensional consolidation [J].
Biot, MA .
JOURNAL OF APPLIED PHYSICS, 1941, 12 (02) :155-164