生态补水以来永定河周边地下水变化分析

Analysis of groundwater change around Yongding River since ecological water replenishment

  • 摘要: 为评估生态补水以来永定河周边地下水的变化,利用空间分析等方法,分析了2019—2022年其地下水水位及水质情况.结果表明:补水期间,永定河沿线地下水水位呈显著回升趋势,其中沿线上游地区回升更为明显;空间上,距离河道越近的区域,地下水水位响应速度越快.研究区地下水呈弱碱性,优势阴阳离子为Ca2+、Na+和\mathrmHCO_3^- .受生态补水、降水、水文地质条件及补水水质等多重因素的共同影响,研究区地下水水质得到了明显的改善,地下水总硬度和硝酸盐氮质量浓度均呈下降趋势,其中硝酸盐氮下降更为显著.

     

    Abstract: To evaluate the variation in groundwater around river course after water replenishment, different methods are used to analyze groundwater level and water quality from 2019 to 2022 around the Yongding River. During water compensation, groundwater level along Yongding River exhibited a significant rebound trend, which is more significant in upstream areas. Spatially, closer the area to the river course, faster is the groundwater level response. The groundwater is weakly alkaline, with Ca2+, Na+ and \mathrmHCO_3^- as the dominant anions and cations. Under combined influence of multiple factors (ecological water replenishment and water quality, precipitation, hydrogeological conditions), the groundwater quality in the study area has improved significantly. Total hardness and nitrate nitrogen concentration of groundwater showed a downward trend, decrease in nitrate nitrogen was particularly significant.

     

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