深层地下热水水位变化的物理化学机理初步探讨
A PRELIMINARY STUDY OF THE PHYSICAL CHEMISTRY MECHANISM OF WATER LEVEL CHANGE OF DEEP THERMO-GROUNDWATER
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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。Abstract: 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.
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[1] 地下水位研究组,地下水位主要干扰因素的识別与地震信息的提取,地震地质,5,4,1983。 [2] H·ф·沃兹娜娅著,水化学与微生物学,中国建筑工业出版社,1983。 [3] K·E·比契叶娃著,水文地球化学,地质出版社,1981。 [4] 堀部纯男等著,海水化学,科学出版社,1983。 [5] 邓禹仁,地热异常区一次强余震的化学热力学背景分析,他震,3,1984。 [6] 温元凯、邵俊,离子极化和离子水化能,科学通报,21,2,1976。 [7] 张正斌、刘莲生,海洋中化学过程的ф(Z/L,x)规律及其应用,科学通报,23, 9, 1978。 -
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