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含孔岩体破裂过程的无单元法数值模拟
引用本文:张 鑫,沈振中,徐力群. 含孔岩体破裂过程的无单元法数值模拟[J]. 河海大学学报(自然科学版), 2008, 36(5): 722-726. DOI: 10.3876/j.issn.1000-1980.2008.05.030
作者姓名:张 鑫  沈振中  徐力群
作者单位:河海大学水利水电工程学院,江苏,南京,210098;河北省水利水电第二勘测设计研究院,河北,石家庄,050021;河海大学水利水电工程学院,江苏,南京,210098
摘    要:根据岩体损伤程度对其渗透性和强度的影响,利用定义的损伤变量建立了应力-渗流-损伤的耦合分析模型.综合考虑应力、渗流、损伤之间的相互作用影响,模拟分析了含孔岩体在不同水压力作用下破裂的过程.分析表明,内水压力是促使裂纹扩展的一个重要因素,内水压力增加可以使原来停止扩展的裂纹重新扩展或者使原来闭合的裂纹重新张开,而且裂纹张开度的变化将导致裂纹内的渗流特性发生改变.

关 键 词:岩体  无单元法  应力-渗流-损伤耦合分析  裂纹扩展
修稿时间:2008-12-04

Numerical simulation of cracking process of rock mass with hole by element-free method
ZHANG Xin,SHEN Zhen-zhong,XU Li-qun. Numerical simulation of cracking process of rock mass with hole by element-free method[J]. Journal of Hohai University (Natural Sciences ), 2008, 36(5): 722-726. DOI: 10.3876/j.issn.1000-1980.2008.05.030
Authors:ZHANG Xin  SHEN Zhen-zhong  XU Li-qun
Abstract:The influence of rock damage degree on the permeability coefficient and intensity of a rock mass was described by defining a damage variable,and a stress-seepage-damage coupling analysis model was established and used to simulate the cracking process of a rock mass with a hole.The results show that the inner water pressure is an important factor in the crack's propagation,and that the increment of inner water pressure can make the crack re-expand,or make the closed crack re-open.It is also indicated that the change of the crack width will result in the change of seepage characteristics within the crack.
Keywords:rock mass  element-free method(EFM)  stress-seepage-damage coupling analysis  crack propagation
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