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湛江市区饮用水源地地下水水化学特征、氮素来源及水质评价

Hydrochemical characteristics, nitrogen sources and water quality evaluation of groundwater in drinking water sources in Zhanjiang City

  • 摘要:
    研究目的 近年来,湛江市区饮用水源地地下水遭受了不同程度的污染,如氮污染等,但其水质现状和氮污染来源不明确,本文旨在探明湛江市区饮用水源地地下水水化学特征及其氮素来源。
    研究方法 通过开展水文地质、水文地球化学结合环境同位素分析等多种手段,明确影响湛江市区浅层、中层与深层3组含水层的水化学特征及主要自然与人为因素和氮素的来源。
    研究结果 湛江市区浅层、中层和深层含水层的补给来源存在水力联系和交换现象。各个含水层的水化学类型的季节性变化不大,浅层含水层水化学类型较复杂,受到较多因素的影响和干扰。研究区浅层水的水岩相互作用以硅酸盐风化和蒸发岩溶解为主,中层水以硅酸盐风化为主,深层水的水岩相互作用以硅酸盐风化和蒸发岩溶解为主,降雨和蒸发对研究区各含水层地下水水质影响均较弱。硝酸盐是浅层和中层含水层主要的无机氮形态,浅层地下水在旱季和雨季均存在氮污染现象,主要来源为化粪池渗滤液和生活污水。但无机氮总体浓度不大,污染较轻。
    结论 湛江市区饮用水源地地下水的水化学类型复杂,主要受控于硅酸盐风化和蒸发岩溶解作用,还受到部分人类活动影响。地下水氨氮和硝酸盐因子超标,加强点位周边生活污水、农业化肥和工业污染源的监管及防治,能有效地保证地下水质量和可持续利用。

     

    Abstract:
    Objective In recent years, the groundwater of drinking water sources in Zhanjiang City has been polluted to varying degrees, such as nitrogen pollution, but its water quality status and nitrogen pollution sources are not clear. The purpose of this paper is to explore the hydrochemical characteristics and nitrogen sources of groundwater in drinking water sources in Zhanjiang City.
    Methods Through various means such as hydrogeological, hydrogeochemical combined with environmental isotope analysis, the hydrochemical characteristics of shallow, middle and deep aquifers in Zhanjiang urban area and the main natural and human factors and nitrogen sources are clearly affected.
    Results There are hydraulic connections and exchange phenomena in the recharge sources of shallow, middle and deep aquifers in Zhanjiang City. The seasonal variation of the hydrochemical types of each aquifer is not large, and the hydrochemical types of the shallow aquifer are more complex, which are affected and interfered by many factors. The water−rock interaction of shallow water in the study area is dominated by silicate weathering and evaporite dissolution, the middle water is dominated by silicate weathering, and the water−rock interaction of deep water is dominated by silicate weathering and evaporite dissolution. Rainfall and evaporation have a weak impact on the groundwater quality of each aquifer in the study area. Nitrate is the main inorganic nitrogen form in shallow and middle aquifers. Shallow groundwater has nitrogen pollution in both dry and rainy seasons. The main sources are septic tank leachate and domestic sewage. However, the overall concentration of inorganic nitrogen is not large and the pollution is light.
    Conclusions The hydrochemical types of groundwater in drinking water sources in Zhanjiang City are complex, mainly controlled by silicate weathering and evaporite dissolution, and also affected by some human activities. Groundwater ammonia nitrogen and nitrate factors exceed the standard. Strengthening the supervision and prevention of domestic sewage, agricultural fertilizer and industrial pollution sources around the site can effectively ensure the quality and sustainable use of groundwater.

     

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