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2022 Vol. 49, No. 6
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XING Yifei, WANG Huiqun, LI Jie, TENG Yanguo, ZHANG Baojian, LI Yanyan, WANG Guiling. 2022. Chemical field of geothermal water in Xiong'an New Area and analysis of influencing factors[J]. Geology in China, 49(6): 1711-1722. doi: 10.12029/gc20220601
Citation: XING Yifei, WANG Huiqun, LI Jie, TENG Yanguo, ZHANG Baojian, LI Yanyan, WANG Guiling. 2022. Chemical field of geothermal water in Xiong'an New Area and analysis of influencing factors[J]. Geology in China, 49(6): 1711-1722. doi: 10.12029/gc20220601
shu

Chemical field of geothermal water in Xiong'an New Area and analysis of influencing factors

  • 1.

    Chinese Academic of Geological Sciences, Beijing 100037, China

  • 2.

    Deep Earth Science and Exploration Technology Laboratory, Ministry of Natural Resources of the People's Republic of China, Beijing 100037, China

  • 3.

    Geothermal and Hot Dry Rock Exploration and Development Technology Innovation Center, Ministry of Natural Resources of the People's Republic of China, Beijing 100037, China

  • 4.

    College of Water Sciences, Beijing Normal University, Beijing 100875, China

    • Fund Project: Supported by the projects of National Key Research and Development (No.2018YFC0604302) and China Geological Survey (No.DD20189114)
More Information
  • Author Bio: XING Yifei, male, born in 1984, Ph.D., senior engineer, mainly engages in geothermal geology and hydrogeology; E-mail: xingyifei@cags.ac.cn
  • Corresponding author: LI Jie, female, born in 1988, Ph.D., lecturer, majors in hydrogeology; E-mail: lijie_lm@163.com 
Received Date:  29 May 2021
Revised Date:  23 September 2021
Publish Date:  25 December 2022
    Abstract

  • This paper is the result of geothermal geological survey engineering.

     Objective

    The hydrochemical formation and evolution of the geothermal water in the Xiong'an New Area have great significant implications to understand the formation mechanism of geothermal resource.

     Methods

    Geothermal water and cold groundwater in the Rongcheng uplift, Niutuozhen uplift, Baxian depression, Baoding depression, and Gaoyang low uplift were sampled for hydrochemical analyses.

     Results

    There are two thermal reservoirs: Sandstone and karst thermal reservoirs. The main hydrochemical types were Cl·HCO3-Na and Cl-Na. The TDS values of geothermal water increased with well depths. Mixing of the geothermal water of the Wumishan Formation and the Guantao Formation was observed in the fault zone. The metamorphic coefficients and desulfurization coefficients of geothermal water in the Wumishan Formation were low, indicating a relatively closed thermal reservoir and reduced state, while the sealing of the reservoirs in the Guantao Formation and Minghuazhen Formation was relatively poor.

     Conclusions

    The chemical field of geothermal water in the study area is controlled by the extent of water-rock interaction, faults, the sealing of the reservoirs, and so on. Our result is of great significance for understanding the geothermal resources in Xiong'an New Area and promoting clean heating in winter in northern China.
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