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EN
The objective of this paper is to present the advantages and problems related to the application of a multi-layer model in hydrogeological investigations, exemplified by the Main Groundwater Basin No. 338. The main aquifer in this basin is Neogene, but Quaternary, Cretaceous and Palaeozoic-Proterozic aquifers have also been identified there. Due to the presence of numerous permeable layers, separated by impermeable ones of irregular distribution in the Neogene aquifer, 27 model layers have been distinguished, including 10 water-bearing horizons. A large number of model blocks caused the increase of the computational time, and a large number of layers have lengthened the calibration time of the model. However, anthropogenic or geologic threats to multi-layer structures have justified such a large number of layers, enabling the water balance for the selected part of the basin orfor the selected depth intervals with groundwater of good or bad status.
EN
The aim of this article is to introduce hydrogeological conditions and possibilities for water consumption in the village Sêkowa near Gorlice where inhabitants are struggling with periodic water service interruptions. There are present solutions to this problem. This object was achieved by the hydrogeological mapping of the terrain and numerical simulation of the hydrogeological conditions and possible options for water take off from the groundwater basin stream Rybnik. The result show that there are effective ways to provide the required amount of water conditions and possible options for water take off from the groundwater basin stream Rybnik. The result show that there are effective ways to provide the required amount of water.
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