东江流域上游赣南地区酸性浅层地下水特征及成因探讨 —以寻乌地区为例
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中国地质调查局长沙自然资源综合调查中心

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中国地质调查局“东江-韩江流域水文地质调查(编号:DD20191019)”和“浙南诸河流域地下水资源调查评价”(编号:DD202111572)项目资助


Characteristics and causes of acidic shallow groundwater in Gannan area in the upper reaches of Dongjiang River Basin ——Take Xunwu area as an example
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Changsha Natural Resources Comprehensive Survey Center,China Geological Survey

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Supported by the “Hydrogeological survey of Dongjiang-Hanjiang River Basin (No.DD2019019)” project of China Geological Survey.

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    摘要:

    【研究目的】东江流域上游赣南地区是我国典型的缺水区,酸性地下水的分布加剧了区域生活用水缺乏程度。【研究方法】本文选择东江流域上游的寻乌地区为研究区,系统采集浅层地下水,采用水化学和数理统计学等方法,分析了酸性地下水的pH值、空间分布、水化学类型的特征,从物质基础、形成环境和人为因素的角度探讨了酸雨、包气带介质、硫化矿物溶解及水化学、人为作用等因素对酸性地下水的控制作用成因。【研究结果】区内地下水pH值集中在5.0~7.0之间;空间分布与地貌特征相关性明显:中低山<丘陵;不同地下水水化学特征都以低矿化度、弱酸性中和能力为主,其pH值,HCO3型(6.0)>HCO3-Cl型(5.05)>SO4型(4.8)>Cl型(4.5);不同介质地下水类型pH值中,碎屑岩类孔隙裂隙水>松散岩类孔隙水>变质岩类裂隙水>岩浆岩类裂隙水。【结论】酸雨和CO2气体的溶解是H+来源的主要物质基础;酸中和能力是影响酸性地下水形成的主要环境,人为因素也是不容忽视的一个要素。研究结果对认识该区酸性地下水成因、合理利用和保护地下水资源具有指导作用。

    Abstract:

    [Objective]Gannan area in the upper reaches of Dongjiang River Basin is a typical water shortage area in China. The distribution of acid groundwater intensifies the lack of regional domestic water. [Methods]This paper selects Xunwu area in the upper reaches of Ganjiang River Basin as the study area, systematically collects shallow groundwater, analyzes the pH value, spatial distribution and hydrochemical type of acid groundwater by using the methods of Hydrochemistry and mathematical statistics, and discusses the control effects of acid rain, aeration zone medium, sulfide mineral dissolution, hydrochemistry and human action on acid groundwater. [Results]The pH value of groundwater in the area is concentrated between 5.0~7.0; The correlation between spatial distribution and geomorphic characteristics is obvious: middle and low mountains < hills; The hydrochemical characteristics of different groundwater are mainly low salinity and weak acid neutralization ability. In pH value, HCO3 type (6.0) > HCO3-Cl type (5.05) > SO4 type (4.8) > Cl type (4.5); Among the pH values of groundwater types in different media, pore fissure water of clastic rock > pore water of loose rock > fissure water of metamorphic rock > fissure water of magmatic rock. [Conclusions]Acid rain and the dissolution of CO2 gas is the main material basis of H+ source; Acid neutralization capacity is the main environment affecting the formation of acid groundwater, and human factors are also an element that can not be ignored. The research results have a guiding role in understanding the causes of acid groundwater, rational utilization and protection of groundwater resources in this area.

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  • 收稿日期:2022-08-05
  • 最后修改日期:2022-11-07
  • 录用日期:2023-05-01
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