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.
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.
出处
《煤炭学报》
EI
CAS
CSCD
北大核心
2000年第1期1-4,共4页
Journal of China Coal Society
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
