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河南淮阳县地热流体化学特征及其成因分析

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文章导航 > 中国地质 > 2022 > 49(3): 956-966

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白博文, 平建华, 赵继昌, 杨振威, 宁艺武, 熊超凡. 2022. 河南淮阳县地热流体化学特征及其成因分析[J]. 中国地质, 49(3): 956-966. doi: 10.2029/gc20220319
引用本文: 白博文, 平建华, 赵继昌, 杨振威, 宁艺武, 熊超凡. 2022. 河南淮阳县地热流体化学特征及其成因分析[J]. 中国地质, 49(3): 956-966. doi: 10.2029/gc20220319
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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
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河南淮阳县地热流体化学特征及其成因分析

  • 1.

    郑州大学水利科学与工程学院, 河南 郑州 450001

  • 2.

    郑州大学地球科学与技术学院, 河南 郑州 450001

  • 3.

    中国地质环境监测院, 北京 100000

  • 基金项目:
    万万江新能源集团有限公司自主研发项目(WJYF2017-21、WJYF2017-23)及河南省中能联建地热工程有限公司自主研发项目(ZNLJYF2018-53)联合资助
详细信息
    作者简介: 白博文, 男, 1994年生, 硕士生, 水文地球化学专业; E-mail: baicurry@163.com
    通讯作者: 平建华, 男, 1976年生, 教授, 从事地热成因、地下水系统研究; E-mail: pingjianhua@zzu.edu.cn

  • 中图分类号: : P314

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)
More Information
    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

    摘要
  • 研究目的

    淮阳地热属于典型的中低温沉降盆地型地热，研究淮阳县地热资源的质与量，有助于其合理开发利用及科学管理。

     研究方法

    本文综合利用地球化学、环境同位素，对淮阳县地温场及地热流体化学特征和成因进行分析研究。

     研究结果

    结果表明，深部热储地温场受基底构造与断裂影响较明显，构造单元分界处和多条断裂交汇处，地温梯度较高，如苏庄地温梯度3.75℃/100 m，其他地段 < 3.5℃/100 m。研究区内地热流体中主要为Cl·HCO3·SO4-Na、Cl·SO4·HCO3－Na、Cl·SO4-Na型。地热流体中阳离子主要以Na+为主，阴离子呈多样化，研究区地热流体主要来源于西部伏牛山区的大气降水，且地热流体发生水-岩作用，但相对较弱。地热流体为1952年前入渗补给的“古水”。

     结论

    淮阳经济可开采热储层主要为新近系明化镇组和馆陶组，区内地热资源开发主要可用来供暖，以促进当地经济发展，助力于本地区“双碳”目标的达成。

    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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  • 图 1  淮阳地质构造图

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  淮阳县南北向地热地质剖面图

    Figure 2. 

    下载: 全尺寸图片 幻灯片

    图 3  淮阳县东西向地热地质剖面图

    Figure 3. 

    下载: 全尺寸图片 幻灯片

    图 4  淮阳县地温梯度等值线图

    Figure 4. 

    下载: 全尺寸图片 幻灯片

    图 5  淮阳地区地热流体水化学类型Piper图

    Figure 5. 

    下载: 全尺寸图片 幻灯片

    图 6  深部地热流体的Caexcess−Nadeficit关系图

    Figure 6. 

    下载: 全尺寸图片 幻灯片

    图 7  离子毫克当量比图

    Figure 7. 

    下载: 全尺寸图片 幻灯片

    图 8  Na-K-Mg平衡图

    Figure 8. 

    下载: 全尺寸图片 幻灯片

    图 9  淮阳地热流体δD与δ18O关系图

    Figure 9. 

    下载: 全尺寸图片 幻灯片

    表 1  井温数据

    Table 1.  Well temperature data

    下载: 导出CSV

    表 2  地热流体水化学分析结果

    Table 2.  Water chemical analysis results of hydrothermal fluids

    下载: 导出CSV

    表 3  Caexcess-Nadeficit数据

    Table 3.  Caexcess-Nadeficit data

    下载: 导出CSV
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收稿日期:  2020-07-02
修回日期:  2020-08-31
刊出日期:  2022-06-25

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