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Recharge of Gdansk municipal groundwater intakes on the Vistula Delta Plain (Northern Poland)

机译:维斯瓦河三角洲平原(波兰北部)的格但斯克市政地下水补给量

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Results of the Vistula Delta Plain Quaternary recharge analysis are presented in this paper. This region is situated south of Gdansk city near the Bay of Gdansk. There are two municipal intakes situated on the Vistula Delta Plain: Lipce and Grodza Kamienna. Different exploitation of the municipal intakes is considered. The numerical calculations are made for the pre-1969 period before the Lipce intake started discharging the Quaternary aquifer in the steady-state conditions and for the 15 years period after the opening of the Lipce intake, in the transient conditions. The results of calculations of the natural state of the Vistula Delta Plain Quaternary aquifer are also presented. The numerical calculations were carried out using the Modflow and Modpath code in Groundwater Modelling System (GMS 2.1) package. Presented results of numerical calculations show that the Quaternary aquifer exploited by groundwater intakes Lipce and Grodza Kamienna is connected with inflow from the Martwa Wisla River into the Vistula Delta Plain Quaternary aquifer and confirm the Quaternary aquifer groundwater flow evaluation based on Cl~- ions concentration in the observation wells.
机译:本文介绍了维斯杜拉三角洲平原第四纪补给分析的结果。该地区位于格但斯克市南部,靠近格但斯克湾。维斯瓦河三角洲平原上有两个市政取水口:里普斯和格罗扎·卡米耶纳。考虑了对市政入口的不同利用。数值计算是在1969年之前的Lipce进气口在稳态条件下开始排放第四层含水层之前,以及在Lipce进气口打开后的15年瞬态条件下进行的。还给出了维斯杜拉河三角洲平原第四纪含水层自然状态的计算结果。数值计算使用地下水建模系统(GMS 2.1)软件包中的Modflow和Modpath代码进行。现有的数值计算结果表明,地下水入水口Lipce和Grodza Kamienna开发的第四层含水层与从Martwa Wisla河流入维斯杜拉三角洲平原第四层含水层的流入有关,并基于Cl〜-离子浓度确定了第四层含水层地下水流量的评估结果。观察井。

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