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裂隙岩体渗流场与应力场耦合数学模型的研究
引用本文:任长吉,黄涛.裂隙岩体渗流场与应力场耦合数学模型的研究[J].武汉大学学报(工学版),2004,37(2):8-12.
作者姓名:任长吉  黄涛
作者单位:1. 吉林大学,吉林,长春,130021
2. 西南交通大学,四川,成都,610031
摘    要:首先研究裂隙岩体中应力场改变对地下水渗流场的影响作用机理,推导出渗透系数k和给水度μ受应力影响的表达式,进而分析渗流场的变化,地下水的作用引起应力场环境变迁,导致裂隙岩体的渗透变形,在此基础上建立了裂隙岩体中应力场与渗流场耦合作用研究工作程式和具"点荷载"特征的等效连续介质耦合数学模型,并应用于一隧道工程实例进行了计算.

关 键 词:裂隙岩体  渗流  应力  耦合  数学模型
文章编号:1671-8844(2004)02-008-05
修稿时间:2003年10月28

A study of mathematical model coupling seepage field and stress field in fractured rock mass
REN Chang-ji,HUANG Tao.A study of mathematical model coupling seepage field and stress field in fractured rock mass[J].Engineering Journal of Wuhan University,2004,37(2):8-12.
Authors:REN Chang-ji  HUANG Tao
Affiliation:REN Chang-ji~1,HUANG Tao~2
Abstract:The thesis studies the mechanism about seepage field changing due to the stress field changing in fractured rock mass; educes the formulae of k and μ that effected by stress; then analyzes the seepage field changing and the stress field changing aroused by effect of groundwater. In this situation, study form of coupling action and coupling mathematical model on equivalent continuum media are presented through theoretical and empirical analysis. Finally, the above mathematical model presented is applied in a tunnel engineering practice.
Keywords:fractured rock mass  seepage  stress  couple  mathematical model
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