高级检索
    付宇, 董好刚, 李立湘, 方泓锦, 袁东方, 周施阳. 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[J]. 中国地质. DOI: 10.12029/gc20220805004
    引用本文: 付宇, 董好刚, 李立湘, 方泓锦, 袁东方, 周施阳. 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[J]. 中国地质. DOI: 10.12029/gc20220805004
    FU Yu, DONG Haogang, LI Lixiang, FANG Hongjin, YUAN Dongfang, ZHOU Shiyang. Characteristics and causes of acidic shallow groundwater in Gannan area in the upper reaches of Dongjiang River Basin ——Take Xunwu area as an example[J]. GEOLOGY IN CHINA. DOI: 10.12029/gc20220805004
    Citation: FU Yu, DONG Haogang, LI Lixiang, FANG Hongjin, YUAN Dongfang, ZHOU Shiyang. Characteristics and causes of acidic shallow groundwater in Gannan area in the upper reaches of Dongjiang River Basin ——Take Xunwu area as an example[J]. GEOLOGY IN CHINA. DOI: 10.12029/gc20220805004

    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

    Characteristics and causes of acidic shallow groundwater in Gannan area in the upper reaches of Dongjiang River Basin ——Take Xunwu area as an example

    • 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、水化学类型及作用特征,从物质基础、循环条件和外部因素的角度探讨了水岩作用、包气带介质、酸雨、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和循环条件相关性明显:中低山<丘陵,补给区<排泄区;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】水岩相互作用是pH值形成和演化主要作用,碳酸离解是H+来源的主要物质基础;包气带介质和酸中和能力是影响酸性地下水形成主要的水循环条件;酸雨和人为因素是不容忽视的外部要素。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: ObjectiveGannan 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. MethodsIn 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 pH value, spatial distribution, hydrochemical types and action characteristics of acidic groundwater are analyzed by using hydrochemistry and mathematical statistics methods. From the point of view of material basis, circulation conditions and external factors, the causes of control of water rock action, aeration zone medium, acid rain, human action and other factors on acidic groundwater are discussed. ResultsThe pH value of groundwater in the area is concentrated between 5.0 and 7.0; The spatial distribution has obvious correlation with geomorphic characteristics and circulation conditions:middle and low mountains3 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.ConclusionsThe interaction between water and rock is the main role in the formation and evolution of pH value, and the dissociation of carbonic acid is the main material basis for the source of H+; Aerated zone medium and acid neutralization ability are the main water circulation conditions affecting the formation of acidic groundwater; Acid rain and human factors are external factors that cannot be ignored. The research results have a guiding role in understanding the origin of acidic groundwater, rational utilization and protection of groundwater resources in this area.

       

    /

    返回文章
    返回