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
- Buneev A. N. To the problem of the origin of mineral waters of Matsesta. Trudy LGGP AN SSSR, vol. II, 1949.
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- Ovchinnikov A. M. Conditions of formation of Matsesta hydrogen sulfide waters. Trudy LGGP AN SSSR, vol. II, 1949.
- Makarenko F. A. On the Genesis of Matsesta hydrogen sulfide waters. Trudy LGGP AN SSSR, vol. II, 1949.
- Pastushenko Yu. N. Buried karst of Upper Jurassic and Cretaceous limestones of the Sochi-Sukhumi area and its hydrogeological significance. Materialy IV konferentsii mladshikh nauchnykh sotrudnikov i aspirantov LGGP AN SSSR. Izdatel'stvo AN SSSR, 1959.
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- Shishokin V. P. Analytical and graphic methods of investigation of equilibrium complex systems. Tsentral'naya laboratoriya fiziko-khimicheskogo analiza AN SSSR, vol. III, iss. 1, 1926.
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