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河南淮阳县地热流体化学特征及其成因分析

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
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

河南淮阳县地热流体化学特征及其成因分析

  • 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

  • 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
  • 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。

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  • 图 1  淮阳地质构造图

    Figure 1. 

    图 2  淮阳县南北向地热地质剖面图

    Figure 2. 

    图 3  淮阳县东西向地热地质剖面图

    Figure 3. 

    图 4  淮阳县地温梯度等值线图

    Figure 4. 

    图 5  淮阳地区地热流体水化学类型Piper图

    Figure 5. 

    图 6  深部地热流体的CaexcessNadeficit关系图

    Figure 6. 

    图 7  离子毫克当量比图

    Figure 7. 

    图 8  Na-K-Mg平衡图

    Figure 8. 

    图 9  淮阳地热流体δD与δ18O关系图

    Figure 9. 

    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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出版历程
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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