Hydrogeologic characteristic of Arakaevskaya parametric well

In the paper, the boundaries and depth of water-bearing units in the Arakaevskaya parametric well are established. The methods of aquifers hydro-chemical composition study and its results are described. Due to occurrence of overthrust structures at the observed area, the allochthon and autochthon water-bearing units are defined. Analysis of hydrodynamic regime showed that the interaction between Urals aquifers and those at the area of study is not observed.