摘要
本文从微观尺度,综合围内外部分有关研究成果并结合一些震例资料,初步分析讨论了由于外界环境因素(温度、压力等)的影响造成地下水本身及其溶液体系内部物理化学性状改变,导致水体积变化,从而引起地下水位变化的各种可能性,也即是热水水位变化的物理化学机理。
Based on summing up, in microscopic scale, of a part of resarch results concerned inside and outside our country and some seismic data, we have preliminarily analysed and discussed the probability that the changes of the physical chemistry property and state of groundwater itself and its solutiowhich are caused by outside environmental factors such as temperature, presn sure and so on might result in a change of water volume and then cause a change of water level. That is the physical chemistry mechanism of water level change of thermowates.
出处
《华北地震科学》
1985年第3期53-58,共6页
North China Earthquake Sciences
