Zobrazeno 1 - 8 of 8 pro vyhledávání: '"E. G. Potapov"'
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Nitrogen and Carbon Isotope Composition of Gases in High-$${{p}_{{{\text{C}}{{{\text{O}}}_{{\text{2}}}}}}}$$ Waters in the North Caucasus
Autor: E. M. Prasolov, E. G. Potapov, V. Yu. Lavrushin, Boris G. Pokrovsky, A. V. Ermakov, A. S. Aydarkozhina
Publikováno v: Geochemistry International. 58:1262-1277
The paper presents the first data on the nitrogen isotope composition of the associated gases of mineral waters in the North Caucasus and newly acquired data on the carbon isotope composition of the CO2 and CH4. Most of the samples were taken from th
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::8873386fb188669ee19e89e18068bb26
https://doi.org/10.1134/s0016702920110087
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4
Analysis of accumulation conditions of minor elements in mineral waters: An example of hydrocarbonate sodic waters of the Nagutskoe mineralized groundwater field
Autor: E. G. Potapov, O. A. Limantseva, S. P. Danilov, E. V. Cherkasova
Publikováno v: Geochemistry International. 54:712-718
Computer simulations of carbon dioxide leaching of Aptian–Albian sandstone at the Nagutskoe groundwater field, Caucasian Mineral Waters, are compared with laboratory experimental data obtained using a high-pressure autoclave under parameters close
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::2774eb4b92691dad2383700ecc7756f9
https://doi.org/10.1134/s001670291608005x
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7
Thermodynamic Simulation of Essentuki Type Mineral Water Formation
Autor: E. G. Potapov, Oxana A. Limantseva
Publikováno v: E3S Web of Conferences, Vol 98, p 05012 (2019)
Thermodynamic models of Essentuki and Nagutsky fields of Caucasian Mineral Waters deposits (KMW) are developed. The models are based on laboratory studies of core samples of aptian-albian lower Cretaceous rock dissolution. The rock samples were disin
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3f4f07e8c35acb17b40e3544d875e55b
https://doi.org/10.1051/e3sconf/20199805012
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