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This paper elaborates the chemical constituent change principles of deep geothermal fluid during the process of upward movement. It summarizes research methods of hydrochemistry, isotope and numerical modelling technique for the physiochemical processes such as decreasing temperature, shallow groundwater infusion, and degassing. The multi-component chemical geothermometry methods including gas geochemical method are discussed. High-temperature geothermal fields in China are mostly located in the southwest with frequent new tectonic movements, especially in Tibet high-temperature geothermal areas. Therefore the paper also focuses the status of high-temperature geothermal fluid research. At last, it's pointed out in the paper that in the future we can start from typical high-temperature geothermal zones and geothermal fields to explore optimization of the multi-component geothermometry method and use it in the reconstruction and analogue of the formation mechanism and internal relevancy of regional geothermal systems.
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篇名 Reconstruction of deep fluid chemical constituents for estimation of geothermal reservoir temperature using chemical geothermometers
来源期刊 地下水科学与工程:英文版 学科 工学
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年,卷(期) dxskxygcywb,(2) 所属期刊栏目
研究方向 页码范围 173-181
页数 9页 分类号 TV
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地下水科学与工程:英文版
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2305-7068
河北省石家庄市中华北大街268号
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