摘要
文中分析了三岔河引子渡电站坝址右岸河间地块岩溶水文地质边界条件，并结合勘探钻孔及连通试验所取得的资料，对该河间地块可疑渗漏地段进行了分析评价，指出了该河间地块地段不存在岩溶管道渗漏的论据。
The paper analyzes karst geohydrological boundary condition of the interstream area on the rightbank of damsite of Yinzidu Hydropower station. Using the data obtained from prospect holing andcommunication tests, appreciating the questionable sections of the interstream area, the writer points outevidences that karst pipe seepage does not exist in the area.
出处
《贵州水力发电》
1999年第1期8-11,共4页
Guizhou Water Power
关键词
引子渡电站
河间地块
岩溶渗漏
Yinzidu Hydropower Station, interstream area, karst seepage
