A linearized porous brittle damage material model with distributed frictional-cohesive faults

被引:22
作者
De Bellis, M. L. [1 ]
Della Vecchia, G. [2 ]
Ortiz, M. [3 ]
Pandolfi, A. [2 ]
机构
[1] Univ Salento, Dipartimento Ingn Innovaz, Lecce, Italy
[2] Politecn Milan, Dipartimento Ingn Civile & Ambientale, Milan, Italy
[3] CALTECH, Engn & Appl Sci Div, Pasadena, CA 91125 USA
关键词
Brittle damage; Multiscale modelling; Recursive faulting; Porous media; Hydraulic conductivity; VARIATIONAL FORMULATION; PERMEABILITY CHANGES; GRANITE; FLOW; DILATANCY; STRESS;
D O I
10.1016/j.enggeo.2016.10.010
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
We present a simplified model of damaging porous material, obtained through consistent linearization from a recursive-faulting material model described in (Pandolfi et al. 2016). The brittle damage material model is characterized by special planar micro-structures, consisting of nested families of equi-spaced frictional cohesive faults in an otherwise elastic matrix material. The linear kinematics model preserves the main microstructural features of the finite kinematics one but offers a far better computational performance. Unlike models commonly employed in geo-mechanical applications, the proposed model contains a small number of parameters, to wit, two elastic moduli, three frictional-cohesive parameters, and three hydraulic response parameters, all of which having clear physical meanings and amenable to direct experimental measurement through standard material tests. The model is validated by comparison to triaxial hydro mechanical experimental data. Despite the paucity of material constants, the salient aspects of the observed behavior are well captured by the model, qualitatively and quantitatively. As an example of application of the model, we simulate the excavation of a borehole in a rocky embankment. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:10 / 24
页数:15
相关论文
共 27 条
[1]  
[Anonymous], 2005, EXPT ROCK DEFORMATIO, DOI [DOI 10.1007/B137431, DOI 10.1007/3-540-26339-X_7]
[2]   Influence of damage on pore size distribution and permeability of rocks [J].
Arson, Chloe ;
Pereira, Jean-Michel .
INTERNATIONAL JOURNAL FOR NUMERICAL AND ANALYTICAL METHODS IN GEOMECHANICS, 2013, 37 (08) :810-831
[3]   PERMEABILITY OF GRANITE UNDER HIGH PRESSURE [J].
BRACE, WF ;
WALSH, JB ;
FRANGOS, WT .
JOURNAL OF GEOPHYSICAL RESEARCH, 1968, 73 (06) :2225-+
[4]   NOTE ON PERMEABILITY CHANGES IN GEOLOGIC MATERIAL DUE TO STRESS [J].
BRACE, WF .
PURE AND APPLIED GEOPHYSICS, 1978, 116 (4-5) :627-633
[5]   A damage model for volcanic edifices: Implications for edifice strength, magma pressure, and eruptive processes [J].
Carrier, Aurore ;
Got, Jean-Luc ;
Peltier, Aline ;
Ferrazzini, Valerie ;
Staudacher, Thomas ;
Kowalski, Philippe ;
Boissier, Patrice .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2015, 120 (01) :567-583
[6]  
Chen WN, 1996, J AM CERAM SOC, V79, P579, DOI 10.1111/j.1151-2916.1996.tb07913.x
[7]   Permeability of triaxially compressed sandstone: Influence of deformation and strain-rate on permeability [J].
Heiland, J .
PURE AND APPLIED GEOPHYSICS, 2003, 160 (5-6) :889-908
[8]   Laboratory testing of coupled hydro-mechanical processes during rock deformation [J].
Heiland, J .
HYDROGEOLOGY JOURNAL, 2003, 11 (01) :122-141
[9]  
Kiyama T., 1996, 2 N AM ROCK MECH S
[10]  
Ma LK, 2012, ROCK MECHANICS: ACHIEVEMENTS AND AMBITIONS, P173