论文部分内容阅读
本文以新安江水电站为例,依据指示剂示踪测试资料并结合地下水动态观测资料,探讨了右岸坝址区厚度很大的非可溶层状岩体中“双重水位”的形成机理及其意义,并分析了区内绕坝渗流的性状。
This paper takes Xin’anjiang Hydropower Station as an example, based on the indicator tracer test data and the dynamic observation data of groundwater, discusses the formation mechanism and significance of “double water level” in non-dissolvable stratiform rock mass with large thickness in right bank dam site , And analyzed the seepage flow characteristics around the dam.