首页 | 本学科首页   官方微博 | 高级检索  
     

降雨入渗下互层状裂隙岩体非饱和渗流分析
引用本文:卢刚,周志芳.降雨入渗下互层状裂隙岩体非饱和渗流分析[J].岩土工程学报,2008,30(9):1399-1403.
作者姓名:卢刚  周志芳
作者单位:河海大学土木工程学院;
摘    要:在总结缓倾状互层裂隙岩体的裂隙发育规律的基础上,给出了其裂隙网络生成方法;介绍了双重介质非饱和渗流理论,并基于此对缓倾状互层裂隙岩体的非饱和渗流场进行了分析,总结了互层状裂隙岩体降雨入渗条件下的非饱和渗流场的一些特征。

关 键 词:层状岩体  双重介质模型  降雨  非饱和渗流场  

Analysis of unsaturated seepage in inter-bed layered fractured rock mass with rainfall infiltration
LU Gang,ZHOU Zhifang.Analysis of unsaturated seepage in inter-bed layered fractured rock mass with rainfall infiltration[J].Chinese Journal of Geotechnical Engineering,2008,30(9):1399-1403.
Authors:LU Gang  ZHOU Zhifang
Affiliation:College of Civil Engineering Hohai University Nanjing 210098 China
Abstract:Based on the review of the fracture development rules in inter-bed layered fractured rock mass,the fracture network generation method was provided,and then the double medium model was introduced.By use of the fracture network and double medium model the unsaturated seepage with rainfall infiltration in inter-bed layered fractured rock mass was analyzed,some characteristics of the unsaturated seepage with rainfall infiltration in inter-bed layered fractured rock mass was summarized.
Keywords:layered rock mass  double medium model  rainfall  unsaturated seepage field
本文献已被 维普 万方数据 等数据库收录!
点击此处可从《岩土工程学报》浏览原始摘要信息
点击此处可从《岩土工程学报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号