Karst hydrogelogical system of the Solotvino deposit, effect of self-tamping of the karst channel and prospects of recovery of speleotherapeutic treatment in mine N9

Abstract

The description of the geological structure, the modern geoecological state, hydrogeological and mining-geological conditions of the Solotvyno salt deposit (Transcarpathian region) is given. Peculiarities of salt karst development are considered and a retrospective analysis of its development within the mine N 9 is carried out: from catastrophic water inflow, active development of technogenic-activated karst and emergency flooding. The effect of self-tamponing of the karst channel in the area of Chorny Mochar was revealed, which allows to predict the possibility of drainage of mine N 9 and restoration of the underground department of the allergy hospital.