摘要
在岩溶地区，利用地下水位观测资料和观测曲线，可以解决很多复杂的岩溶水文地质问题，笔者提出的利用岩溶地下水位动态曲线和洪枯地下水位变幅以及地表水位和地下水位错峰时间来分析岩溶水文地质条件的几种新方法，综合称为岩溶地下水位动态分析法，用以评价岩溶发育程度、岩体透水性以及水库岩溶渗漏等问题。
Many complicated karst hydrogeologic problems can be resolved by analysing groundwa- ter level data and curves, In order to evaluate degree of karstification, rock mass permeability and reservior leakage the author put forward several methods for analysing karst hydrogeo- logic conditions using karst groundwater level fluctuation curves,amplitude of groundwater level fluctuation during flood and drought periods,and difference in time for surface and ground water peak level.All these are termed the methods of analysis of karst groundwater level fluctuation.
出处
《中国岩溶》
CAS
CSCD
北大核心
1995年第3期261-269,共9页
Carsologica Sinica
关键词
岩溶地区
地下水
水位动态
karst groundwater level fluctuation
unsymmetry coefficient
karst leakage.
