大区域裂隙岩体渗流水电比拟实验技术的研究  

Study of Experimental Technicality of Electric Analog Model for Seepage in Large Zones

作　　者：赵坚[1] 速宝玉[1] 杨晓文 

机构地区：[1]河海大学水利水电工程学院

出　　处：《水利水电科技进展》1998年第6期36-40,共5页Advances in Science and Technology of Water Resources

基　　金：电力科学技术发展基金

摘　　要：介绍利用水电比拟模型研究大区域裂隙岩体渗流问题的实验方法，对实验中遇到的如区域交形过分，分离变界面连接等问题，提出了看法和解决途径。与水力学网络模型实验结果比较表明，用水电比拟模型研究大区域裂隙岩体渗流问题是可行和简便的。The paper presents the experimental method of electric analog model used for studying seepage of fissured rock masses in large zones.Methods are proposed to solve the problems of deformity zone and connection of separated boundaries with occur in experiment.Compared with experimental results obtained for hydraulic model of fissure network,the results from the electric analog model for the study of the seepage of fissured rock masses in large zones indicate that the method is very simple and practical.

关 键 词：渗流 水电比拟模型 裂隙 岩体 连续介质 

分 类 号：TU452[建筑科学—岩土工程] O357[建筑科学—土工工程]