Groundwaters which occur at a deep depth of Devonian formations have a high temperature (42-54°C) and character of brine (M=89,19-167,84 g/dm3). Filtration parameters and groundwater recharge are weakly recognized. Measurements of confined groundwater surface led to errors because these waters have variable density. In this conditions only reduction of measure groundwater pressure permit to calculate filtration. Application of mathematical modelling make possible to describe groundwater circulation, water balance and estimate to renewable and disposable groundwater resources.
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