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    丹阳市吕城地区浅层地下水演化特征及成因

    Evolution characteristics and genesis of shallow groundwater in Lücheng area of Danyang City

    • 摘要: 在野外调查和取样分析的基础上,运用统计学、Piper三线图、Gibbs模型及相关性分析等方法对丹阳市吕城地区浅层地下水水化学特征、类型及成因进行了分析。结果表明:该区浅层地下水pH值变化较小,属于中性偏弱碱性水;阳离子中Ca2+、Na+占主导优势,阴离子中HCO3-占绝对优势;水化学类型主要有HCO3-Ca型、HCO3-Ca·Na型、HCO3·SO4-Ca·Na型、HCO3·Cl-Ca·Na型和HCO3-Ca·Na·Mg型。近年来浅层地下水TDS呈现降低趋势,表明存在一定程度的淡化现象。分析发现,第四纪沉积环境、岩石风化作用、水文地质条件与人类经济活动等综合作用是该区浅层地下水演化特征及其差异性的主要原因。

       

      Abstract: Based on the field investigation and sampling analysis, the hydrochemical characteristics, types and genesis of shallow groundwater in Lücheng area of Danyang City were analyzed by using the methods of statistics, Piper trigram, Gibbs model and correlation analysis.The results show that the pH value of shallow groundwater in this area has little change, belonging to neutral and slightly alkaline water. Ca2+ and Na+ were dominant in cations, while HCO3- was the absolute dominant in anion.The main hydrochemical types are HCO3-Ca, HCO3-Ca·Na, HCO3·SO4-Ca·Na, HCO3·Cl-Ca·Na and HCO3-Ca·Na·Mg. In recent years, TDS of shallow groundwater shows a decreasing trend, indicating a certain degree of desalination phenomenon. It is found that the comprehensive effects of Quaternary sedimentary environment, rock weathering, hydrogeological conditions and human economic activities are the main reasons leading to the evolution characteristics and differences of shallow groundwater in this area.

       

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