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岩体裂隙网络非线性渗流分析
引用本文:柴军瑞. 岩体裂隙网络非线性渗流分析[J]. 水动力学研究与进展(A辑), 2002, 17(2): 217-221
作者姓名:柴军瑞
作者单位:四川大学水电学院,四川成都,610065,西安理工大学水电学院,陕西西安,710048
基金项目:中国博士后科学基金资助项目 (2 0 0 1年第 2 9批 )
摘    要:裂隙中水流为紊流状态时,流量与水力坡度呈非线性关系,不再满足线性的立方定律,以岩体裂隙网络中结点的水量平衡来建立岩体裂缝网络非线性渗流控制方程式,提出矩阵求解方法和迭代运算步骤,并给出应用算例与验证。算例结果表明,不能采用岩体裂隙网络线性渗流规律来代替岩体裂隙网络非线性渗流规律。

关 键 词:岩体 裂隙网络 渗流 非线性 紊流 水力坡度 水利工程
文章编号:1000-4874(2002)02-0217-05
修稿时间:2000-12-24

Analysis of nonlinear seepage through fracture network in rock mass
CHAI Jun-rui . Analysis of nonlinear seepage through fracture network in rock mass[J]. Chinese Journal of Hydrodynamics, 2002, 17(2): 217-221
Authors:CHAI Jun-rui
Affiliation:CHAI Jun-rui 1,2
Abstract:The flow rate is nonlinearly related to the hydraulic gradient when fluid flow through the fracture network in rock mass is turbulence. The governing equations for seepage through fracture network in rock mass were establised based on water balance at nodes, and the matrix solution method and the iterative steps were proposed. An example was also given to show that the law for seepage through fracture network in rock mass cannot be approximately regarded as the linear one.
Keywords:rock mass  fracture network  seepage  nonlinearity
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