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Hydrochemical Characteristics and Multivariate Statistical Analysis of Natural Water System: A Case Study in Kangding County, Southwestern China

机译:天然水系统的水化学特征和多元统计分析:以西南康定县为例

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The utilization for water resource has been of great concern to human life. To assess the natural water system in Kangding County, the integrated methods of hydrochemical analysis, multivariate statistics and geochemical modelling were conducted on surface water, groundwater, and thermal water samples. Surface water and groundwater were dominated by Ca-HCO 3 type, while thermal water belonged to Ca-HCO 3 and Na-Cl-SO 4 types. The analyzing results concluded the driving factors that affect hydrochemical components. Following the results of the combined assessments, hydrochemical process was controlled by the dissolution of carbonate and silicate minerals with slight influence from anthropogenic activity. The mixing model of groundwater and thermal water was calculated using silica-enthalpy method, yielding cold-water fraction of 0.56–0.79 and an estimated reservoir temperature of 130–199 °C, respectively. δD and δ 18 O isotopes suggested that surface water, groundwater and thermal springs were of meteoric origin. Thermal water should have deep circulation through the Xianshuihe fault zone, while groundwater flows through secondary fractures where it recharges with thermal water. Those analytical results were used to construct a hydrological conceptual model, providing a better understanding of the natural water system in Kangding County.
机译:水资源利用一直是人类生活中极为关注的问题。为了评估康定县的天然水系统,对地表水,地下水和热水样品进行了水化学分析,多元统计和地球化学建模的综合方法。地表水和地下水以Ca-HCO 3类型为主,而热水则分别为Ca-HCO 3和Na-Cl-SO 4类型。分析结果总结了影响水化学成分的驱动因素。根据综合评估的结果,通过人为活动的轻微影响,碳酸盐和硅酸盐矿物的溶解控制了水化学过程。利用二氧化硅-焓法计算了地下水和热水的混合模型,得出的冷水分数分别为0.56-0.79,估计的储层温度为130-199°C。 δD和δ18 O同位素表明,地表水,地下水和温泉是陨石起源的。温泉水应在咸水河断裂带深层循环,而地下水则流经二次裂缝,并在其中补充热水。这些分析结果被用来构建水文概念模型,以更好地了解康定县的自然水系统。

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