Natural dilution of mineral waters of Matsesta
Authors:
Abstract
As is known, the 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 fractures and karst passages. Dilution processes at Matsesta have affected the water‑bearing limestone strata to a depth of about 900 m. The dynamics of this process has been studied in great detail, and the hydrochemistry is still not sufficiently clear and understood ...
Область исследования:
(Archived) Without section
Funding:
None
References
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