Natural depletion of mineral waters of Matsesta
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Abstract
As it is known, mineral waters of Matsesta are diluted with fresh waters of meteoric origin at a considerable depth. The main mass of fresh water enters the depths of the deposit from the north-east, from the zone of the Akhshtyr, Akhun and Bytkha ridges, through a system of open cracks and karst passages. Dilution processes at Matsesta have captured the water-bearing limestone strata to a depth of about 900 meters. The dynamics of this process has been studied in great detail, and the hydrochemistry is still not sufficiently clear and understood ...
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References
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