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2022 Vol. 49, No. 3
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BAI Bowen, PING Jianhua, ZHAO Jichang, YANG Zhenwei, NING Yiwu, XIONG Chaofan. 2022. Chemical characteristics and causes analysis of the geothermal fluid in Huaiyang County, Henan Province[J]. Geology in China, 49(3): 956-966. doi: 10.2029/gc20220319
Citation: BAI Bowen, PING Jianhua, ZHAO Jichang, YANG Zhenwei, NING Yiwu, XIONG Chaofan. 2022. Chemical characteristics and causes analysis of the geothermal fluid in Huaiyang County, Henan Province[J]. Geology in China, 49(3): 956-966. doi: 10.2029/gc20220319
shu

Chemical characteristics and causes analysis of the geothermal fluid in Huaiyang County, Henan Province

  • 1.

    School of Water Conservancy Engineering, Zhengzhou University, Zhengzhou 450001, Henan, China

  • 2.

    The School of Earth Science and Technology, Zhengzhou University, Zhengzhou 450001, Henan, China

  • 3.

    China Institute of Geo-Environment Monitoring, Beijing 10000, China

    • Fund Project: Supported by the independent R & D project of Wanjiang New Energy Group Co., Ltd. (No. wjyf2017-21, No. wjyf2017-23) and the independent R & D project of Henan Zhongneng LianJian Geothermal Engineering Co., Ltd. (No. znljyf2018-53)
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  • Author Bio: PING Jianhua, male, born in 1976, professor, engaged in geothermal genesis and groundwater system; E-mail: baicurry@163.com
  • Corresponding author: PING Jianhua, male, born in 1976, professor, engaged in geothermal genesis and groundwater system; E-mail: pingjianhua@zzu.edu.cn 
Received Date:  02 July 2020
Revised Date:  31 August 2020
Publish Date:  25 June 2022
    Abstract

  • This paper is result of geothermal geological survey engineering

     Objective

    Geothermal resource in Huaiyang area belongs typical medium- low temperature geothermal resource of subsidence basin. Evaluation of geothermal resources in the Huaiyang area can provide insights into its exploitation and scientific management.

     Methods

    In this paper, we analyzed the geochemical and isotopes characteristics of geothermal fluids to explore their local geothermal field features and genesis.

     Results

    The results show that the deep thermal reservoirs are significantly affected by basement structure and faults characteristics. The geothermal gradient is higher (e.g., 3.75℃/100m in the Suzhuang area) along the boundary of faults than the other areas (e.g., 3.5℃/100m). The type of the geothermal fluids are dominated by Cl · HCO3 · SO4-Na, Cl·SO4·HCO3－Na and Cl·SO4-Na. The main cation of the geothermal fluid is Na+ while the anions variou in types. The geothermal fluids were probably derived from the atmospheric "ancient water" of the Funiu Mountain in the western Henan province before 1952, with relatively weak rock-fluid reaction.

     Conclusions

    The major exploited geothermal reservoirs are placed at the Neogene Minghuazhen and Guantao Formations. The geothermal resources are mainly used for heating feeding, etc., which has greatly improved the local economy, Contribute to the realization of the "dual carbon" goal in the region.
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