西藏林周县地下水-地表水化学特征、成因及水质评价

    Chemical characteristics, genesis and water quality assessment of groundwater and surface water in Linzhou County, Xizang

    • 摘要:
      研究目的 林周县作为西藏拉萨河流域的核心区域,其地下水和地表水是重要的饮用水源和生态因子。近年来,人类活动和气候变化对区域水环境的影响日益显著。本文旨在揭示林周县水化学形成机制,评估水质现状,为高原水资源保护提供科学依据。
      研究方法 采集37组水样,测定31项水化学指标,综合运用数理统计、Piper图、Gibbs图、离子比例系数等方法分析水化学特征及成因,并采用单指标最高类别法和模糊数学法进行水质评价。
      研究结果 研究区水质为弱碱性淡水,优势离子为HCO3、SO42−、Ca2+和Mg2+,水化学类型主要为HCO3−Ca和HCO3•SO4−Ca型,地下水和地表水化学组成高度相关;水化学组分主要受岩石风化作用控制,硅酸盐岩和碳酸盐岩风化是主要来源,其成因与区内岩浆岩、变质岩和碳酸岩地质成因相关;模糊数学法水质评价显示,Ⅰ类水占比87%,Ⅱ类5%,Ⅲ类8%,无Ⅳ、Ⅴ类水,单指标最高类别法评价出硝酸盐、氨氮、锰和砷4项指标为主控指标,硝酸盐、氨氮受农业活动影响,锰、砷超标与原生地球化学背景有关。
      结论 林周县水质整体优良,但需关注局部区域农业污染和原生地质成因重金属的影响,研究结果可为高原水资源管理和生态保护提供理论支撑。

       

      Abstract:
      Objective Linzhou County is the core area of Lhasa River Basin in Xizang. Groundwater and surface water are important drinking water sources and ecological factors in this area.In recent years, the impacts of human activities and climate change on the regional water environment have become increasingly pronounced. This study aims to elucidate the hydrochemical formation mechanisms in Linzhou County, assess current water quality conditions, and provide a scientific basis for water resource protection in plateau regions.
      Methods A total of 37 water samples were collected, and 31 hydrochemical parameters were measured. Comprehensive analytical methods, including mathematical statistics, Piper diagrams, Gibbs diagrams, and ion ratio coefficients, were employed to investigate hydrochemical characteristics and formation mechanisms. Water quality was evaluated using both the Single Indicator Highest Category Method and the Fuzzy Mathematics Method.
      Results The water quality in the study area is characterized as weakly alkaline freshwater, with dominant ions being HCO3, SO42−, Ca2+and Mg2+ ions. The hydrochemical types of water are mainly HCO3−Ca and HCO3•SO4−Ca, demonstrating a strong correlation between groundwater and surface water chemistry. The hydrochemical composition is predominantly governed by rock weathering processes, with silicate and carbonate weathering serving as the principal sources, linked to the geological origins of magmatic, metamorphic, and carbonate rocks in the region.Based on the Fuzzy Mathematics Evaluation Method, water quality classification revealed that 87% of samples met Class Ⅰ standards, 5% were Class Ⅱ, and 8% were Class Ⅲ, with no samples falling into Class Ⅳ or Ⅴ. The Single Indicator Highest Category Method identified nitrate, ammonia nitrogen, manganese, and arsenic as the dominant controlling factors. Elevated nitrate and ammonia nitrogen levels were primarily attributed to agricultural activities, while manganese and arsenic exceedances were associated with natural geochemical background conditions.
      Conclusions The overall water quality in Linzhou County remains excellent; however, localized agricultural pollution and geogenic heavy metals require targeted attention.These findings provide a theoretical foundation for water resource management and ecological conservation in high−altitude regions.

       

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