吴家庄水库库区岩溶渗漏分析  

ANALYSIS OF KARSTIC LEAKAGE IN WUJIAZHUANG RESERVIOR AREA

作　　者：李桂平[1] 安民[1] 王延涛[1] 王丽丽[1] 韩锐敏[1] 

机构地区：[1]水利部山西水利水电勘测设计研究院,太原030024

出　　处：《工程地质学报》2000年第3期334-336,共3页Journal of Engineering Geology

摘　　要：吴家庄水库位于山西省黎城县境内 ,拟建于由西南源和北源汇合而成的浊漳河干流上 ,总库容 3.6亿 m3,属大型水利工程。坝址区基岩为震旦系串岭沟组石英砂岩 ,向上游库区依次出露寒武、奥陶系碳酸盐岩 ,其分布面积占整个库区面积的一半以上 ,岩溶渗漏是库区最主要的工程地质问题 ,它直接影响到建库规模的确定和工程的可行性 ,本文就此进行了分析、评价 。Wujiazhuang Reservoir is located in Licheng County of Shanxi Province. It was designed to be constructed on Zhuozhang River confluent of the southwest basin and north basin. Its total capacity is 360 mullion cubic meters and will be a large-scale hydroelectric project. The bedrocks at the dam site are hard quartz sandstone of Chuanlinggou Formation of Sinian system and the Cambrian and Ordovician carbonate rocks. Cover more than 50% of the total reservoir area. The karstic leakage is a most significant engineering geological problem. It can directly affect the reservoir site and the feasibility of project. This paper presents a corresponding analysis and an evaluation of the condition and then a recommendation of the rexervoir sizes and capacity.

关 键 词：吴家庄水库 浊漳河 岩溶 渗漏 

分 类 号：P642.254[天文地球—工程地质学]