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四川昭觉地区优质偏硅酸地下水的特征、成因及其开发利用建议

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周长松, 邹胜章, 朱丹尼, 林永生, 王佳, 樊连杰, 李军, 蓝芙宁, 李衍青, 邓日欣, 缪雄谊. 2022. 四川昭觉地区优质偏硅酸地下水的特征、成因及其开发利用建议[J]. 中国地质, 49(3): 849-859. doi: 10.12029/gc20220312
引用本文: 周长松, 邹胜章, 朱丹尼, 林永生, 王佳, 樊连杰, 李军, 蓝芙宁, 李衍青, 邓日欣, 缪雄谊. 2022. 四川昭觉地区优质偏硅酸地下水的特征、成因及其开发利用建议[J]. 中国地质, 49(3): 849-859. doi: 10.12029/gc20220312
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ZHOU Changsong, ZOU Shengzhang, ZHU Danni, LIN Yongsheng, WANG Jia, FAN Lianjie, LI Jun, LAN Funing, LI Yanqing, DENG Rixin, MIAO Xiongyi. 2022. Characteristics, causes and development suggestions of high quality groundwater containing metasilicate in Zhaojue area, Sichuan Province[J]. Geology in China, 49(3): 849-859. doi: 10.12029/gc20220312
Citation: ZHOU Changsong, ZOU Shengzhang, ZHU Danni, LIN Yongsheng, WANG Jia, FAN Lianjie, LI Jun, LAN Funing, LI Yanqing, DENG Rixin, MIAO Xiongyi. 2022. Characteristics, causes and development suggestions of high quality groundwater containing metasilicate in Zhaojue area, Sichuan Province[J]. Geology in China, 49(3): 849-859. doi: 10.12029/gc20220312
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四川昭觉地区优质偏硅酸地下水的特征、成因及其开发利用建议

  • 1.

    中国地质科学院岩溶地质研究所 自然资源部/广西壮族自治区岩溶动力学重点实验室 广西岩溶资源环境工程技术研究中心, 广西 桂林 541004

  • 2.

    中国矿业大学环境与测绘学院, 江苏 徐州 221116

  • 3.

    河北建筑工程学院 河北省水质工程与水资源综合利用重点实验室, 河北 张家口 075000

  • 基金项目:
    广西重点研发计划(桂科AB21220044、桂科AB21075002、桂科AB18050026)、国家研发计划课题(2017YFC0406104)、国家自然科学基金(41902261)、中国地质调查局地质调查项目(DD20190825, DD20160302、DD20221758)、中国地质科学院岩溶地质研究所基本科研业务费项目(2021013)共同资助
详细信息
    作者简介: 周长松, 男, 1987年生, 硕士, 助理研究员, 主要从事岩溶区水文地质环境地质; E-mail: changsongzhou@karst.ac.cn
    通讯作者: 邹胜章, 男, 1969年生, 博士, 研究员, 主要从事岩溶区水文地质环境地质; E-mail: zshzh@karst.ac.cn

  • 中图分类号: P632;P596

Characteristics, causes and development suggestions of high quality groundwater containing metasilicate in Zhaojue area, Sichuan Province

  • 1.

    Key Laboratory of Karst Dynamics of Ministry of Land and Resources, Guangxi Karst Resources and Environment Research Center of Engineering Technology, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, Guangxi, China

  • 2.

    School of Environment Science and Spatial Informatics, China University of Mining and Technology, Xuzhou 221116, Jiangsu, China

  • 3.

    Hebei Key Laboratory of Water Quality Engineering and Comprehensive Utilization of Water Resources, Hebei University of Architecture, Zhangjiakou 075000, Hebei, China

  • Fund Project: Supported by the Key Research and Development Program of Guangxi (No.GuikeAB21220044, No. GuikeAB21075002, No. GuikeAB18050026), the National Key Research and Development Program of China(No. 2017YFC0406104), the National Natural Science Foundation for Young Scholars of China(No. 41902261), the project of China Geological Survey(No. DD20190825, No. DD20160302, No. DD20221758), and the Basic Research Projects of the Institute of Karst Geology, Chinese Academy of Geological Sciences (No.2021013)
More Information
    Author Bio: ZHOU Changsong, male, born in 1987, assistant researcher, mainly engaged in the study of hydrogeological environment geology in karst rrea; E-mail: changsongzhou@karst.ac.cn .
    Corresponding author: ZOU Shengzhang, male, born in 1969, researcher, mainly engaged in the study of hydrogeological environment geology in karst rrea; E-mail: zshzh@karst.ac.cn

    摘要
  • 研究目的

    近年来，随着生活水平的不断提高，人们对健康饮水的要求也在不断提高，寻找与开发富含H2SiO3等矿物质优质地下水已成为关键。

     研究方法

    本文以昭觉地区水文地质调查工程、地下水污染调查工程所获取的地下水化学数据为基础，探讨了昭觉地区富H2SiO3地下水的分布特点、元素水文地球化学特征、形成条件及成因。

     研究结果

    结果显示：（1）全县富H2SiO3（≥25 mg/L）地下水均属于低矿化度偏碱性水，分布在基底岩石为玄武岩的6个片区，H2SiO3含量一般介于25.74~46.04 mg/L，pH含量一般介于7.4~8.58，TDS含量一般介于49.4~333 mg/L；（2）玄武岩地下水存在HCO3-Ca、HCO3-Ca·Mg、HCO3-Ca·Na、HCO3-Ca·Mg·Na、HCO3-Na等5种水化学类型，总体以HCO3－Ca·Mg为主，其次为HCO3-Ca，再次为HCO3-Ca·Na，三者分别占总采样点数的50.00%、25.76%、12.12%；（3）全县富H2SiO3地下水的形成受水岩相互作用、硅酸盐矿物的分布范围及其可溶性、围岩裂隙发育程度、水源涵养及补给条件等四方面因素影响，其中水岩相互作用占据主导作用；（4）在后续开发利用过程中，需进一步揭示影响地下水中H2SiO3分布与迁移的因素。

     结论

    研究结果可以为昭觉地区矿泉水产业的发展及城乡优质水源地的建设提供依据。

    This paper is the result of hydrogeological survey engineering.

     Objective

    In recent years, the drinking water health issues has been taken due to the improvement of living standards. Finding and developing high- quality groundwater with high- level minerals (e.g. H2SiO3) has become the key step in improving human health.

     Methods

    The hydrogeological survey and groundwater pollution survey were carried out in the Zhaojue County, and the spatial distributions of H2SiO3-rich groundwater, hydrogeochemical components characteristics and factors were revealed.

     Results

    The main results including: (1)The groundwater with H2SiO3 (≥ 25mg/L) was identified as the low salinity and alkaline water, which distributed in the six areas with the basement rocks of basalt. The H2SiO3 concentration was generally 25.74-46.04 mg/L, pH level was generally 7.4- 8.58, and TDS level is generally 49.4- 333 mg/L; (2)The H2SiO3- rich groundwater of study area was characterized by the low mineralization while the main hydrochemical types of groundwater are HCO3- Ca·Mg and HCO3- Ca; (3) The H2SiO3- rich groundwater was influenced by the water- rock interactions, the distribution range and solubility of silicate minerals, the development of surrounding rock fissures, and water conservation and recharge conditions in the county, among which the water- rock interactions play a critical role; (4) It is necessary to further reveal the main factors affecting the distribution and migration of H2SiO3 in groundwater in the subsequent development and utilization process.

     Conclusions

    The results can provide a basis for the development of mineral water industry and the construction of urban and rural high-quality water sources in Zhaojue area.
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  • 图 1  昭觉县区域地质背景简图

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  昭觉县地下水H2SiO3分布图

    Figure 2. 

    下载: 全尺寸图片 幻灯片

    图 3  研究区玄武岩区水化学类型状况图

    Figure 3. 

    下载: 全尺寸图片 幻灯片

    图 4  昭觉县玄武岩区地下水Twater与H2SiO3关系曲线图（N=45）

    Figure 4. 

    下载: 全尺寸图片 幻灯片

    表 1  昭觉主要含水岩组地下水H2SiO3含量（mg/L）分布特征参数统计结果

    Table 1.  Eigenvalue statistics of H2SiO3 concentration(mg/L)in the main water-bearing rock formations in Zhaojue County

    下载: 导出CSV

    表 2  研究区水化学组分相关系数矩阵（N=12）

    Table 2.  Correlation coefficient of hydrochemical parameters of study area

    下载: 导出CSV
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收稿日期:  2020-04-01
修回日期:  2022-05-10
刊出日期:  2022-06-25

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