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黄河水资源是沿黄地区经济和社会发展的重要限制因子。由于黄河在下游河段形成地上悬河,黄河的侧渗成为该地区地下水的重要补给源。通过分析温县的含水层结构,建立了地下水的二维模型,应用feflow软件对温县的浅层地下水进行了模拟,并对不同黄河水位变化情况下的黄河侧渗量进行了模拟计算,认为随着黄河水位的变化,将会引起两岸地下水位的相应变化,这为该县的水资源管理提供了依据。
The Yellow River water resources are an important limiting factor for economic and social development along the Yellow River. As the Yellow River formed in the lower reaches of the hanging river, the Yellow River’s infiltration of groundwater as an important source of recharge in the area. By analyzing the aquifer structure in Wenxian County, a two-dimensional model of groundwater was established. The shallow groundwater in Wenxian County was simulated by feflow software and the Yellow River lateral infiltration volume under different Yellow River water level changes was simulated. With the change of the Yellow River water level, corresponding changes in the groundwater level across the Taiwan Strait will be caused, which provides the basis for the county’s water resources management.