Chistyakova N.F.






Graduated from Kiev State University named after T.G. Shevchenko (1971), specialization “organic chemist”.
PhD in Geological and Mineralogical Sciences, Professor.
Professor of the Department of Geoecology and Environmental Management, Institute of Earth Sciences (INZEM), Tyumen State University.
Scientific interest area: water and hydrocarbon fluids, their chemical composition; geotemperature field and fluid dynamics of productive deposits of oil and gas basins.
Author of more than 250 publications.
Geochemical research
Section editor – PhD in geology and mineralogy Bazhenova T.K.
Article # 30_2020 submitted on 12/27/2019 displayed on website on 09/23/2020
20 p.
pdf Features of the brine water composition of the Vendian - Lower Cambrian Middle Botuoba oil-gas-condensate field during the catagenesis time
The salt water omposition of underground brines of the Vendian - Lower Cambrian sections of the Middle Botuoba oil-gas-condensate field during the catagenesis stage is considered; the peculiarity of which is the presence of polygenic waters in certain block traps of B5 and Б1 levels: sodium sulfate, sodium hydrogencarbonate and chlorine-magnesium genetic types together with the prevailing chlorine-calcium genetic type. The zoning of the groundwater of the strata by mineralization and four genetic types of groundwater has been carried out. The directions of water entry into the reservoirs formed at the stage of catagenesis and entering together with hydrocarbons in the corresponding traps are established. It is shown that, while maintaining the mechanism of formation of the salt water composition in the "rock-water" system, the polygenicity of the formation waters present simultaneously in one reservoir layer reflects a regular change in the components of their chemical composition during the transition from the artesian basin to the oil and gas basin. The most sensitive ions of the chemical composition of groundwater, reflecting the transition of the artesian basin to the new geological state of the catagenesis stage, are sulfate, bicarbonate, and sodium ions.

Keywords: groundwater, ion-salt water composition, rock-water system, water genetic types, polygenic water, hydrochemical inversion, Middle Botuoba oil-gas-condensate field.
article citation Chistyakova N.F. Dravante V.V., Sivtsev A.I. Osobennosti ionno-solevogo sostava podzemnykh vod vend-nizhnekembriyskikh otlozheniy Srednebotuobinskogo neftegazokondensatnogo mestorozhdeniya na stadii katageneza [Features of the brine water composition of the Vendian - Lower Cambrian Middle Botuoba oil-gas-condensate field during the catagenesis time]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 3, available at: http://www.ngtp.ru/rub/2020/30_2020.html
DOI https://doi.org/10.17353/2070-5379/30_2020
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