摘要
本文概述了利用理论模型和水井气压效应及固体潮效应三种反演含水层应力变化的方法。分别给出了这三种井水位阶变与其含水层所受的应力之间的定量关系,讨论了这三个方法的可行性和优缺点。
This paper sums up three methods of inversion of stress changes of aquifers using theoretical results, the effect of well barometric pressures and the effect of the earth tide responses and presents respectively the quantitative relationship between the step changes of the three types of well water tables and the stress on the aquifers. The paper also discusses the feasibility and advantages and disadvantages of these three methods.
出处
《华北地震科学》
北大核心
1993年第1期39-44,共6页
North China Earthquake Sciences
