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Numerical modeling of permeability evolution based on degradation approach during progressive failure of brittle rocks

Numerical modeling of permeability evolution based on degradation approach during progressive failure of brittle rocks

作     者:Zhang Chunhui Yue Hongliang Zhao Quansheng Wang Laigui 

作者机构:School of Civil Engineering Hebei University of Science and Technology Shijiazhuang 050018 China School of Mechanics and Engineering Liaoning Technical University Fuxin 123000 China 

出 版 物:《International Journal of Mining Science and Technology》 (矿业科学技术学报(英文版))

年 卷 期:2016年第26卷第4期

页      面:535-542页

核心收录:

学科分类:08[工学] 080104[工学-工程力学] 0815[工学-水利工程] 0801[工学-力学(可授工学、理学学位)] 

基  金:the National Natural Science Foundation of China (Nos.51274079,51274110 and 51574139) the Natural Science Foundation of Hebei Province (No.E2013208148) 

主  题:Hoek Brown failure criterion Dilatancy Permeability evolution Confining pressure Degradation of strength 

摘      要:The permeability evolution of rock during the progressive failure process is described. In combination with the strength degradation index, the degradation formulas of s and a, which are dependent on the plastic confining strain component, the material constants of Hock-Brown failure criterion are presented, and a modified elemental scale elastic-brittle-plastic constitutive model of rock is established. The rela- tionship between volumetric strain and permeability through tri-axial compression is investigated. Based on the above, a permeability evolution model is established. The model incorporates confining pressure- dependent degradation of strength, dilatancy and corresponding permeability evolution. The model is implemented in FLAC by the FISH function method. The permeability evolution behavior of rock is inves-tigated during the progressive failure process in a numerical case. The results show that the model is cap- able of reproducing, and allowing visualization of a range of hydro-mechanical responses of rock. The effects of confining pressure on degradation of strength, dilatancy and permeability evolution are also reflected.

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