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利用钻入承压含水层的深井水位对固体潮和气压的响应来求含水层参数,最早是由Bre-dehoeft (1967)提出的。由于所得的孔隙率等参数是水文地质学家们感兴趣而又不易得到的,地球物理学家则对用含水层的弹性参数来解释固体潮响应感兴趣,所以这个问题受到重视并相继进行探讨。但是深入考查有关主要文献,发现至今这个问题并未得到很好解决。为促进这项研究,现将主要作者的基本假设和公式作一简要介绍并提出粗浅评论。
The determination of aquifer parameters using the response of deep tide wells drilled into confined aquifers to solid tides and pressures was first proposed by Bre-dehoeft (1967). Because of the porosity and other parameters that are of interest to hydrogeologists and not readily available, geophysicists are interested in interpreting the tidal response using the elastic parameters of the aquifer, so this issue has received much attention and has been explored . However, in-depth examination of the main literature, found that so far this problem has not been well resolved. To facilitate this research, we present a brief introduction of the basic assumptions and formulas of the lead authors and make superficial comments.