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平阴-东阿水文地质单元岩溶地下水化学特征分析

齐欢   

  • 出版日期:2020-06-28 发布日期:2020-06-28

Analysis on chemical characteristics of karst groundwater in Pingyin-Dong’e hydrogeological unit

QI Huan   

  • Online:2020-06-28 Published:2020-06-28

摘要: 为研究平阴-东阿水文地质单元地下水化学特征,采用相关性分析法、因子分析法、聚类分析法等方法对研究区26组岩溶地下水样的10项指标进行了综合分析。结果表明:研究区地下水化学类型以HCO3-Ca·Mg和HCO3-Ca为主;地下水在补给区、径流区和排泄区水化学成分呈现明显的差异性。控制岩溶地下水成分的主要因素是NO-3,SO42-,Na+和Ca2+,可以反映样本71.20%的信息量;其中,NO-3和SO42-主要受工矿生产和人类活动的影响,贡献率为31.98%;Na+主要受人类活动的影响,贡献率为22.65%;Ca2+主要受灰岩的风化-溶滤作用影响,贡献率为20.17%。

关键词: 水化学特征, 岩溶地下水, 平阴-东阿水文地质单元

Abstract: 10 indicators of 26 groups of karst groundwater samples in the study area were comprehensively analyzed to study the groundwater chemical characteristics of the Pingyin-Dong'e hydrogeological unit by correlation analysis, factor analysis and cluster analysis. The results showed that the groundwater hydrochemical types in the study area were dominated by HCO3-Ca·Mg and HCO3-Ca. The chemical composition of groundwater in the recharge, runoff and discharge areas showed significant differences. The main factors controlling the composition of karst groundwater were NO-3, SO42-, Na+ and Ca2+, which can reflect 71.20% of the information volume of the sample. NO-3 and SO42- were mainly affected by industrial production and human activities, with a contribution rate of 31.98%. Na+ was mainly affected by human activities, with a contribution rate of 22.65%. Ca2+ was mainly affected by the weathering-solubility of limestone, and with a contribution rate of 20.17%.