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    东江流域上游赣南地区地下水水化学特征及酸性地下水成因探讨——以寻乌地区为例

    Characteristics and causes of acidic shallow groundwater in Gannan area in upper reaches of Dongjiang River Basin: Taking Xunwu area as an example

    • 摘要:
      研究目的 东江流域上游赣南地区是中国典型的缺水区,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,分析了地下水的水化学特征,包括pH值、空间分布、水化学类型及作用特征,并从水循环角度探讨了酸性地下水的成因,包括大气降水(酸雨和人类活动影响)、包气带特征、含水层岩性及水岩相互作用。
      研究结果 研究区内地下水pH值集中在5.0~7.0,整体呈酸性;空间分布与地貌特征和循环条件相关性明显:中低山<丘陵,补给区<排泄区;水化学类型以低矿化度HCO3型为主,但酸性中和能力较弱,其pH值表现为HCO3型(6.0)>HCO3−Cl型(5.05)>SO4型(4.8)>Cl型(4.5);不同含水介质中,碎屑岩类孔隙裂隙水pH值最高,岩浆岩类裂隙水最低。
      结论 酸性地下水是水化学特征的重要表现,其成因主要受水循环过程控制:酸雨入渗是H+的主要来源,包气带缓冲能力弱和含水层酸中和能力低是重要的循环条件,水岩相互作用中硫化物氧化贡献显著,而碳酸离解作用相对次要。酸雨和人为活动是重要的外部影响因素。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:
      This paper is the result of hydrogeological survey engineering.
      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 In this paper, Xunwu area in the upper reaches of the Dongjiang River basin is selected as the study area. Shallow groundwater is systematically collected, and the hydrochemical characteristics including pH value, spatial distribution, hydrochemical types and action characteristics are analyzed by using hydrochemistry and mathematical statistics methods. From the perspective of water cycle, the causes of acidic groundwater are discussed, including atmospheric precipitation (acid rain and human activities), aeration zone characteristics, aquifer lithology and water-rock interaction.
      Results The pH value of groundwater in the area is concentrated between 5.0 and 7.0, showing overall acidity; The spatial distribution has obvious correlation with geomorphic characteristics and circulation conditions: middle and low mountains<hills, recharge area<discharge area; The hydrochemical types are dominated by low salinity HCO3 type with weak acid neutralizing capacity. Its pH value is HCO3 type (6.0)>HCO3−Cl type (5.05)>SO4 type (4.8)>Cl type (4.5); Among different aquifer media, the pH value of pore fissure water of clastic rock is the highest, while that of fissure water of magmatic rock is the lowest.
      Conclusions Acidic groundwater is an important manifestation of hydrochemical characteristics, and its origin is mainly controlled by water cycle process: acid rain infiltration is the main source of H+, weak buffer capacity of aeration zone and low acid neutralization capacity of aquifer are important circulation conditions, sulfide oxidation in water-rock interaction contributes significantly, while carbonic acid dissociation is relatively secondary. Acid rain and human activities are important external influencing factors. The research results have a guiding role in understanding the origin of acidic groundwater, rational utilization and protection of groundwater resources in this area.

       

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