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Propagation simulation and dilatancy analysis of rock joint using displacement discontinuity method 被引量:4

Propagation simulation and dilatancy analysis of rock joint using displacement discontinuity method
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摘要 A revised displacement discontinuity method(DDM) program is developed for the simulation of rock joint propagation and dilatancy analysis. The non-linear joint model used in the program adopts Barton-Bandis normal deformation model, Kulhaway shear deformation model and Mohr-Coulomb criterion. The joint propagation criterion is based on the equivalent stress intensity factor which can be obtained by regression analysis. The simulated rock joint propagation accords well with the existing knowledge. The closure and opening of joint is investigated by DDM, and it is shown that if the opening volume of propagated joint is larger than closure volume of the old joint, the joint dilatancy occurs. The dilatancy condition is mainly controlled by the normal stiffness of the rock joint. When the normal stiffness is larger than the critical value, joint dilatancy occurs. The critical normal stiffness of rock joint changes with the joint-load angle, and joint dilatancy is most possible to occur at 30°. A revised displacement discontinuity method (DDM) program is developed for the simulation of rock joint propagation and dilatancy analysis. The non-linear joint model used in the program adopts Barton-Bandis normal deformation model, Kulhaway shear deformation model and Mohr-Coulomb criterion. The joint propagation criterion is based on the equivalent stress intensity factor which can be obtained by regression analysis. The simulated rock joint propagation accords well with the existing knowledge. The closure and opening ofj oint is investigated by DDM, and it is shown that if the opening volume of propagated joint is larger than closure volume of the old joint, the joint dilatancy occurs. The dilatancy condition is mainly controlled by the normal stiffness of the rock joint. When the normal stiffness is larger than the critical value, joint dilatancy occurs. The critical normal stiffness of rock joint changes with the joint-load angle, and joint dilatancy is most possible to occur at 30°.
出处 《Journal of Central South University》 SCIE EI CAS 2014年第3期1184-1189,共6页 中南大学学报(英文版)
基金 Project(2009318000046) supported by the Western Transport Technical Program of the Ministry of Transport,China
关键词 位移不连续法 传播模拟 岩石节理 MOHR-COULOMB准则 扩容 应力强度因子 程序开发 变形模型 joint propagation joint dilat:mcy displacement discontinuity method non-linear rock joint numerical simulation
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