Experimental evidence on formation of imminent and short-term hydrochemical precursors for earthquakes

被引:21
|
作者
Du, Jianguo [1 ,2 ]
Amita, Kazuhiro [2 ]
Ohsawa, Shinji [2 ]
Zhang, Youlian
Kang, Chunli [3 ]
Yamada, Makoto [2 ]
机构
[1] China Earthquake Adm, Inst Earthquake Sci, Beijing 100036, Peoples R China
[2] Kyoto Univ, Inst Geothermal Sci, Beppu, Oita 8740903, Japan
[3] China Earthquake Adm, China Earthquake Network Ctr, Beijing 100036, Peoples R China
关键词
CHEMICAL-CHANGES; THERMAL SPRINGS; GROUNDWATER; TAIWAN; HYDROGEOCHEMISTRY; CHINA; JAPAN; WATER; FAULT;
D O I
10.1016/j.apgeochem.2010.01.015
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The formation of imminent hydrochemical precursors of earthquakes is investigated by the simulation for water-rock reaction in a brittle aquifer. Sixty-one soaking experiments were carried out with granodiorite and trachyandesite grains of different sizes and three chemically-distinct waters for 6 to 168 h. The experimental data demonstrate that water-rock reaction can result in both measurable increases and decreases of ion concentrations in short times and that the extents of hydrochemical variations are controlled by the grain size, dissolution and secondary mineral precipitation, as well as the chemistry of the rock and groundwater. The results indicate that water-rock reactions in brittle aquifers and aquitards may be an important genetic mechanism of hydrochemical seismic precursors when the aquifers and aquitards are fractured in response to tectonic stress. (C) 2010 Elsevier Ltd. All rights reserved.
引用
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页码:586 / 592
页数:7
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