Abstract
It is shown the possibility of water supply of Mykolayiv at the expense of underground waters of the Upper Sarmatian aquifer in the case of emergencies. Hydrogeological model of the Mykolayiv groundwater field has been developed. The structure of water exchange and the sources of formation of the underground water resources of the Upper Sarmatian aquifer, the main aquifer of drinking groundwater in the vicinity of Mykolayiv, have been studied. The influence of various factors on water-content of the Upper Sarmatian deposits, including protection of drinking underground waters from pulling brackish waters from the Bug estuary was analysed. The possibility of forced exploitation of groundwater of this horizon, depending on the duration of the emergency period, has been studied.
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