摘要
非饱和带裂隙中的饱和区和排干区可以用一个离散的气-水界面分隔开。此气-水界面的位置可以用边界元数值方法通过迭代确定,这样就可以实现对单裂隙内非饱和渗流的描述。将此数值方法推广到裂隙网络中,为用离散裂隙网络模型模拟裂隙岩体非饱和渗流提供了初步的框架。几个算例的计算结果验证了计算程序的正确性。
A numerical method for fluid flow in unsaturated fissures is presented. The capillary theory and the unsaturated flow features for unsaturated fracture are studied simultaneously. A discrete air-water interface is used to separate the saturated zones from the drained zones within each single fracture of fracture network. A numerical method is developed to look for the position of the equilibrium air-water interface by using the Newton-Raphson iteration scheme, which can give a frame for modeling unsaturated flow in fractured rocks with the discrete fracture network models.
出处
《岩石力学与工程学报》
EI
CAS
CSCD
北大核心
2004年第19期3252-3257,共6页
Chinese Journal of Rock Mechanics and Engineering
基金
国家自然科学基金(50128908)
国家重点基础研究发展规划(973)项目(2002CB412707)资助课题
关键词
水力学
非饱和裂隙
渗流
气-水界面
Flow of fluids
Fracture mechanics
Interfaces (materials)
Numerical methods