Microcrack-based coupled damage and flow modeling of fracturing evolution in permeable brittle rocks

被引:101
作者
Lu, Y. L. [1 ,2 ]
Elsworth, D. [2 ]
Wang, L. G. [1 ]
机构
[1] China Univ Min & Technol, State Key Lab Geomech & Deep Underground Engn, Xuzhou 221008, Jiangsu, Peoples R China
[2] Penn State Univ, Ctr & Energy & Mineral Engn G3, EMS Energy Inst, University Pk, PA 16802 USA
关键词
Microcracks; Damage; Hydro-mechanical coupling; Finite element method; Hydraulic fracturing; TRIAXIAL COMPRESSION TESTS; LOCAL DEGRADATION APPROACH; FLUID-FLOW; STATISTICAL TECHNIQUES; MICROMECHANICAL MODEL; ANISOTROPIC DAMAGE; FAILURE; MECHANICS; HETEROGENEITY; STRESS;
D O I
10.1016/j.compgeo.2012.11.009
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
Microcracks in brittle rocks affect not only the local mechanical properties, but also the poroelastic behavior and permeability. A continuum coupled hydro-mechanical modeling approach is presented using a two-scale conceptual model representing realistic rock material containing micro-fractures. This approach combines a microcrack-based continuous damage model within generalized Biot poroelasticity, in which the tensors of macroscopic elastic stiffness, Biot effective stress coefficient and of overall permeability are directly related to microcrack growth. Heterogeneity in both mechanical and hydraulic properties evolves from an initially random distribution of damage to produce localized failure and fluid transmission. A significant advantage of the approach is the ability to accurately predict the evolution of realistic fracturing and associated fluid flow in permeable rocks where pre-existing fractures exert significant control. The model is validated for biaxial failure of rock in compression and replicates typical pre- and post-peak strength metrics of stress drop, AE event counts, permeability evolution and failure modes. The model is applied to the simulation of hydraulic fracturing in permeable rocks to examine the effects of heterogeneities, permeability and borehole pressurization rate on the initiation of fracturing. The results indicate that more homogenous rocks require higher hydraulic pressure to initiate fracturing and breakdown. Moreover, both the fracturing initiation pressure and breakdown pressure decrease with permeability but increase with borehole pressurization rate, and the upper and lower limit of the initiation pressure are seen to be given by the impermeable (Hubbert-Willis) and permeable (Haimson-Fairhurst) borehole wall solutions, respectively. The numerical results are shown to be in good agreement with the experimental observations and theoretical results. This coupled damage and flow modeling approach provides an alternative way to solve a variety of complicated hydro-mechanical problems in practical rock engineering with the process coupling strictly enforced. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:226 / 244
页数:19
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