节点文献
节理岩体中地下水流动的离散元模拟
Modelling of ground water flow in jointed rock masses with distinct element method
【摘要】 地下水在节理岩体中流动时,会引起岩体中应力场与渗流场的相互作用.以节理开度变化为纽带,进行了岩体中渗流场与应力场的耦合分析,并用离散元法完成了计算,给出了计算实例.
【Abstract】 When ground water flows in jointed rock mass, it will cause the interaction between stress field and seepage field in the rock mass Joint aperture is used as a connection for coupled analysis of seepage and stress, and discrete element method is adopted to complete such analysis Computational examples are presented.
【关键词】 节理岩体;
渗流;
节理开度;
数值模拟;
【Key words】 jointed rock mass; seepage; joint aperture; numerical modelling;
【Key words】 jointed rock mass; seepage; joint aperture; numerical modelling;
【基金】 国家自然科学基金! (49772 1 67);地质灾害防治与地质环境保护国家专业实验室基金
- 【文献出处】 煤炭学报 ,JOURNAL OF CHINA COAL SOCIETY , 编辑部邮箱 ,2000年01期
- 【分类号】P641.2
- 【被引频次】31
- 【下载频次】449