上海地区潜水水化学特征与成因机制

    Hydrochemical characteristics and formation mechanisms of phreatic groundwater in Shanghai

    • 摘要:
      研究目的 潜水水环境对于上海生态之城建设具有重要意义,弄清不同沉积环境下潜水水环境特征与形成机理对水资源管理方式的优化和水土环境治理工作模式的确立具有很好的参考价值。
      研究方法 通过对上海地区102口潜水监测井开展地下水样品采集和分析测试,开展基于地下水化学方法的地下水环境成因和演化机制研究。
      研究结果 研究结果表明,研究区潜水pH值在6.93~8.23之间,呈中—弱碱性,TDS普遍小于1000 mg/L。湖积平原区和滨海平原区潜水水化学特征差异较小,三角洲平原区潜水在主要离子含量、水化学类型上较其它2个沉积区有一定差异。3个沉积区潜水水化学成因基本相似,均以水-岩作用为主,并受蒸发作用影响。沿江沿海区域潜水受海水入侵影响不明显。正向阳离子交换反应是影响潜水水化学演化的重要因素,潜水普遍受到人类活动影响。
      结论 根据研究区潜水水环境特征和成因机制,提出3类沉积环境的地下水管理方式和水土环境治理工作模式的建议。湖积平原区和滨海平原区水土环境治理工作宜以解决点状问题为主,三角洲平原区不宜布局污染型产业,水土环境治理工作需要点、面结合,并以区域性治理为主。

       

      Abstract:
      Objective  Phreatic groundwater environment is critical to Shanghai’s establishment as an ecological city. Clarifying the characteristics and formation mechanisms of the phreatic groundwater environment in different sedimentary settings provides valuable reference for optimizing water resource management approaches and establishing soil−water environmental governance frameworks.
      Methods  This study conducted sampling and analytical testing of groundwater samples from 102 phreatic groundwater monitoring wells in Shanghai area, and carried out research on the origin and evolution mechanisms of the groundwater environment based on hydrochemical methods.
      Results  The results show that the pH of phreatic groundwater in the study area ranges from 6.93 to 8.23, indicating neutral to weakly alkaline, with TDS generally below 1000 mg/L. The hydrochemical characteristics of phreatic groundwater in the lacustrine plain area and the coastal plain area show minor differences, while the phreatic groundwater in the delta plain area exhibits certain variations in major ion concentrations and hydrochemical types compared to the other sedimentary areas. The hydrochemical origins of phreatic groundwater in the three sedimentary areas are fundamentally similar, primarily dominated by water−rock interactions and influenced by evaporation. Phreatic groundwater in areas along the river and coast shows no significant impact from seawater intrusion. Positive cation exchange is an important factor influencing the hydrochemical evolution of phreatic groundwater. Phreatic groundwater is generally affected by human activities.
      Conclusions Based on the characteristics and formation mechanisms of the phreatic groundwater environment in the study area, this study proposes recommendations for groundwater management approaches and soil−water environmental governance frameworks for the three types of sedimentary environments. In lacustrine plain and coastal plain, soil and water environmental remediation should primarily focus on addressing point−source pollution. In delta plain, polluting industries should be avoided, and remediation efforts require a combination of point−source and area−wide approaches, with emphasis on regional−scale management.

       

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