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    陕西省勉县矿泉水化学特征及形成机制

    Chemical characteristics and formation mechanism of mineral water in Mianxian county, Shaanxi province

    • 摘要: 本研究以陕西省勉县矿泉水为对象,系统开展了其水化学特征与形成机制分析。基于区内56组水样的系统采集与水化学测试数据,综合运用自组织地图(SOM)与k均值聚类、Piper三线图、相关性分析、矿物饱和指数(SI)及离子比例分析等方法,主要取得以下认识:(1)揭示了研究区矿泉水的水化学类型组合与空间分异特征:区内矿泉水以HCO3-Ca型为主,整体呈中性至弱碱性,属低矿化度淡水。SOM聚类将水样划分为6类,其空间分布格局清晰指示了水岩相互作用(Cluster 1, 3, 4)、局部蒸发浓缩(Cluster 5, 6)及混合稀释作用(Cluster 2)的差异性影响。(2)综合多源证据辨析了控制水化学演化的关键机制:矿物饱和指数与离子比例分析共同证实,碳酸盐矿物的溶解-沉淀平衡是主导水化学组成的主要过程;铝硅酸盐矿物(特别是长石类)的风化则构成了重要的离子补给来源,体系风化程度已达以高岭石为产物的中级阶段;局部水体的蒸发浓缩与大气降水混合是导致水质空间分异的重要次生过程。本研究明确了勉县矿泉水以天然水岩相互作用为核心、多过程耦合的形成机制,为该区域矿泉水资源的评价、开发与保护提供了科学依据。

       

      Abstract: This study systematically investigated the hydrochemical characteristics and formation mechanism of mineral water in Mianxian County, Shaanxi Province. Based on systematic collection and hydrochemical analysis of 56 water samples from the area, integrated application of Self-Organizing Map (SOM) combined with k-means clustering, Piper trilinear diagrams, correlation analysis, mineral Saturation Index (SI) calculations, and ion ratio analysis, the main findings are as follows: (1) The hydrochemical type assemblages and spatial differentiation characteristics of the mineral water in the study area were revealed. The mineral water is predominantly of the HCO3-Ca type, generally neutral to weakly alkaline, and classified as fresh water with low total dissolved solids. SOM clustering categorized the water samples into six clusters, with their spatial distribution patterns clearly indicating the differential influences of water-rock interactions (Cluster 1, 3, 4), localized evaporation-concentration (Cluster 5, 6), and mixing-dilution processes (Cluster 2). (2) The key mechanisms controlling the hydrochemical evolution were identified by synthesizing multiple lines of evidence. Both mineral saturation indices and ion ratio analyses confirm that the dissolution-precipitation equilibrium of carbonate minerals is the predominant process governing the hydrochemical composition. The weathering of aluminosilicate minerals (particularly feldspars) constitutes a significant source of ion replenishment, with the weathering system having reached an intermediate stage where kaolinite is the stable product. Local evaporation-concentration and mixing with atmospheric precipitation are important secondary processes responsible for the spatial heterogeneity of water quality. This study elucidates the formation mechanism of mineral water in Mianxian, which is centered on natural water-rock interactions and coupled with multiple processes, providing a scientific basis for the evaluation, development, and protection of mineral water resources in the region.

       

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