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节理岩质边坡地下水渗流的离散元分析

Analysis of Underground Water Flow in Jointed Rock Slope with the Distinct Element Method

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【作者】 王艳丽王勇许建聪伍国军

【Author】 WANG Yan-li1,2,WANG Yong 3,XU Jian-cong1,2,WU Guo-jun 3(1.Department of Geotechnical Engineering,Tongji University,Shanghai 200092,China;2.Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education,Tongji University,Shanghai 200092,China;3.Institute of Rock and Soil Mechanics,Chinese Academy of Sciences,State Key Laboratory and Geotechnical Engineering,Wuhan 430071,China)

【机构】 同济大学地下建筑与工程系中国科学院武汉岩土力学研究所岩土力学与工程国家重点实验室

【摘要】 从岩体裂隙网络渗流的特点出发,以节理开度变化为纽带,对裂隙岩体渗流场与应力场耦合的离散裂隙网络模型进行分析,采用离散单元法对节理岩质边坡不同库水位条件下的渗流场与应力场进行了耦合分析,比较真实地模拟了库水位上升对节理岩质边坡渗流场与应力场的改造,研究了库水位上升对边坡变形和稳定性的影响规律。结果表明:水库蓄水后,随着水位的抬升,坡体内的最大位移、最大孔压、最大流量均有不同程度的增大,而边坡的稳定性逐渐降低。

【Abstract】 Based on the postulate of the characteristics of fluid flow through joint networks of rock mass and taking the change of the joint width as a link,the fracture network model of the coupled seepage and stress fields in fractured rock mass is studied.The raising of the reservoir water level behind the jointed rock slope is simulated,the deformation trends of the coupling of stress and seepage is studied and the change of the slope stability under different water levels is gained.The results show that with the raising of the water level,the maximal displacement,the maximal pore pressure and the maximal flow rate are increasing to different extent and the slope stability is decreasing.

【基金】 中国博士后科学基金资助项目(20060390165);上海市博士后科研资助计划资助项目(06R214152)
  • 【文献出处】 地下空间与工程学报 ,Chinese Journal of Underground Space and Engineering , 编辑部邮箱 ,2008年04期
  • 【分类号】TU457
  • 【被引频次】26
  • 【下载频次】628
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