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裂隙岩体渗流新模型
引用本文:李定方,鄢俊,陶同康.裂隙岩体渗流新模型[J].水利水运工程学报,1996,0(4).
作者姓名:李定方  鄢俊  陶同康
作者单位:南京水利科学研究院水工研究所
基金项目:“八五”国家科技攻关资助项目
摘    要:为适应网状和层状渗透结构,根据多边形裂隙网络理论.确立了裂隙网络生成的原理和方法,系统地推导了在渗流和应力耦合作用下裂隙岩体渗流模型。并结合拉西瓦水电站坝区岩体裂隙构造的特征,进行了渗流计算和分析;还与连续介质和裂隙网络渗流模型进行了计算比较。

关 键 词:岩体,裂隙,渗流,等势线,数学模型

A new model on seepage through fissured rock mass
Li Dingfang,Yan Jun,Tao Tongkang.A new model on seepage through fissured rock mass[J].Hydro-Science and Engineering,1996,0(4).
Authors:Li Dingfang  Yan Jun  Tao Tongkang
Affiliation:Naming Hydraulic Research Institute
Abstract:In this paper,a new model is completely derived on seepage through fissured rock mass under the coupled action of seepage and stress.To suit the needs of netted and stratified structures,principle and methods for producing fissured network are determined for the computation of seepage according to polygon fissured network theory.In the light of tectonic characteristics of rock fracture in the Laxiwa dam area,computation and analysis of seepage are fully conducted. Compared with porous media seepage model and fissured network seepage model,the present model shows its superiority.
Keywords:rock mass  fissuring  seepage  equipotential line  mathematic model
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