广东湛江市东北部地下水质量、主要影响因素及其开发利用潜力

    Groundwater quality and main influencing factors in the northeast of Zhanjiang City, Guangdong Province

    • 摘要:
      研究目的 查明湛江东北部沿海地区地下水质量并研究其主要影响因素、成因及开发利用潜力,为区域水资源开发利用及保护管理提供理论依据。
      研究方法 在研究区采集50个地下水全分析样, 现场检测168口民井的pH值。综合运用舒卡列夫分类法、描述性统计分析、Pearson相关关系分析、Gibbs图、离子端元法、离子比值法等方法评价地下水水质并划分等级,分析影响地下水质量的主要因素及地下水开发利用潜力。
      研究结果 综合评价显示,地下水水质以Ⅳ类、Ⅴ类为主,物源分析显示地下水化学主要受硅酸盐矿物分化影响,其次为大气降水。酸性降雨、含水介质酸缓冲能力、地层中的铁质矿物、河流及海水的潮汐作用综合影响了区内地下水的pH值;地下水中Fe、Mn呈强正相关关系,含水介质为地下水中的Fe、Mn提供了物源基础,溶滤作用、酸性地下水环境及还原环境影响了Fe、Mn含量;Se来源主要为鉴江上游的富硒砂页岩,同时受地下水酸碱环境、Fe含量等因素的影响,其对地下水质量的影响尚不明确。研究区地下水具有较大的开发潜力,且吴川市地下水开发潜力大于坡头区。
      结论 研究区地下水质量主要影响因素为pH、铁(Fe)、锰(Mn)、硒(Se),这些因素受原生地质环境、区域水文地质条件和气候环境综合影响。松散岩类孔隙潜水适宜分散性开采,松散岩类孔隙承压水适宜集中开采,可加强对吴川市地下水资源的开发。

       

      Abstract:
      Objective Investigate the quality of groundwater in the northeastern coastal area of Zhanjiang, study the formation mechanisms of its main influencing factors, and assess its development and utilization potential, providing a theoretical basis for regional water resource development, utilization, and protection management.
      Methods A total of 50 groundwater samples were collected within the area for comprehensive analysis, and pH levels were measured on−site in 168 private wells. Groundwater quality was evaluated and classified using a combination of methods including Shukalev classification, descriptive statistical analysis, Pearson correlation analysis, Gibbs diagrams, end−member mixing analysis, and ion ratio methods. The study analyzed the formation mechanisms of key factors affecting groundwater quality and assessed the potential for groundwater development and utilization.
      Results The comprehensive evaluation indicates that groundwater quality is predominantly classified as Class IV and Class V. Source analysis shows that the groundwater chemistry is primarily influenced by the weathering of silicate minerals, followed by atmospheric precipitation. The pH of groundwater in the area is jointly affected by acid rain, the acid buffering capacity of the aquifer media, iron−bearing minerals in the strata, and tidal influences from rivers and seawater. Iron (Fe) and manganese (Mn) in groundwater exhibit a strong positive correlation; the aquifer media provide the source material for Fe and Mn, while leaching processes, acidic groundwater conditions, and reducing environments control their concentrations. Selenium mainly originates from selenium−enriched sandstone and shale in the upper reaches of Jianjiang River, and its concentration is also influenced by the groundwater's pH and Fe content. The impact of selenium on groundwater quality remains unclear. The study area holds significant groundwater development potential. , with Wuchuan City having greater potential than Potou District.
      Conclusions The primary factors affecting groundwater quality in the study area are pH, iron (Fe), manganese (Mn), and selenium (Se), which are collectively influenced by the native geological environment, regional hydrogeological conditions, and climatic factors. Loose rock−type pore water is suitable for dispersed extraction, while loose rock−type pore confined water is suitable for centralized extraction, facilitating enhanced development of underground water resources in Wuchuan City.

       

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