鄱阳湖环湖区浅层地下水化学特征及形成机制
Hydrochemical characteristics and formation mechanism of shallow groundwater in around-lake area of Poyang Lake
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摘要: 为研究鄱阳湖环湖区浅层地下水化学特征及形成机制,综合应用Piper三线图法、聚类分析法、离子比例系数法等方法,对研究区内242组地下水水样的14项指标进行系统分析。研究结果表明:研究区浅层地下水属于总硬度偏低的弱酸性淡水,地下水中阳离子以Ca2+为主,阴离子以HCO-3为主;Piper三线图表明,研究区浅层地下水水化学类型以HCO3-Ca型、HCO3-Ca·Mg型、HCO3-Na·Ca型和HCO3·Cl-Na·Ca型为主;聚类分析法和离子比例系数法表明,研究区浅层地下水水化学组分受矿物风化溶解作用影响较大,蒸发浓缩和阳离子交换作用相对较弱。Abstract: To investigate the hydrochemical characteristics and formation mechanism of shallow groundwater in the around-lake area of Poyang Lake,14 indicators of 242 groups of groundwater samples were analyzed by Piper diagram,cluster analysis and iron ration analysis.The results showed that the groundwater belonged to the weakly acidic fresh water with low total hardness;Ca2+ was the dominant cation in groundwater,HCO3- was the dominant anion.Piper diagram showed that the hydrochemical types of groundwater were mainly HCO3-Ca,HCO3-Ca·Mg,HCO3-Na·Ca and HCO3·Cl-Na·Ca.Cluster analysis and ion ration analysis showed that the groundwater chemical compositions were mainly affected by rock weathering and dissolution,partly affected by evaporation-concentration and cation exchange.
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