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Role of water-rock interactions in the formation of the composition of radon waters of the Zaeltsovsky field (the southern part of West Siberia). / Novikov, D. A.; Dultsev, F. F.; Chernykh, A. V.

в: Journal of Physics: Conference Series, Том 1451, № 1, 012007, 09.09.2020.

Результаты исследований: Научные публикации в периодических изданияхстатья по материалам конференцииРецензирование

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Novikov DA, Dultsev FF, Chernykh AV. Role of water-rock interactions in the formation of the composition of radon waters of the Zaeltsovsky field (the southern part of West Siberia). Journal of Physics: Conference Series. 2020 сент. 9;1451(1):012007. doi: 10.1088/1742-6596/1451/1/012007

Author

Novikov, D. A. ; Dultsev, F. F. ; Chernykh, A. V. / Role of water-rock interactions in the formation of the composition of radon waters of the Zaeltsovsky field (the southern part of West Siberia). в: Journal of Physics: Conference Series. 2020 ; Том 1451, № 1.

BibTeX

@article{63624240747547d08f42cc1472d5bfbb,
title = "Role of water-rock interactions in the formation of the composition of radon waters of the Zaeltsovsky field (the southern part of West Siberia)",
abstract = "Results of thermodynamic calculations of the interactions of radon waters from the Zaeltsovsky field with the minerals of host rocks are presented for the first time. It was established that waters under study are supersaturated with respect to calcite and siderite, and to a smaller extent with respect to magnesite and dolomite. No saturation of radon waters with respect to primary aluminosilicate minerals (albite, anortite, microcline, ferrosilite) is observed. The points are located in the fields of stability of clayey minerals (kaolinite, Ca- and Mg-montmorillonite, Fe-sepiolite), gibbsite and leptochlorite. In the evolution of the water-rock system, they correspond to the siallite type of interaction with rocks. ",
keywords = "equilibrium, hydrogeochemistry, Novosibirsk, radon waters, water-rock system, Western Siberia",
author = "Novikov, {D. A.} and Dultsev, {F. F.} and Chernykh, {A. V.}",
year = "2020",
month = sep,
day = "9",
doi = "10.1088/1742-6596/1451/1/012007",
language = "English",
volume = "1451",
journal = "Journal of Physics: Conference Series",
issn = "1742-6588",
publisher = "IOP Publishing Ltd.",
number = "1",
note = "2nd International Conference on Applied Physics, Power and Material Science, ICAPPM 2019 ; Conference date: 20-12-2019 Through 21-12-2019",

}

RIS

TY - JOUR

T1 - Role of water-rock interactions in the formation of the composition of radon waters of the Zaeltsovsky field (the southern part of West Siberia)

AU - Novikov, D. A.

AU - Dultsev, F. F.

AU - Chernykh, A. V.

PY - 2020/9/9

Y1 - 2020/9/9

N2 - Results of thermodynamic calculations of the interactions of radon waters from the Zaeltsovsky field with the minerals of host rocks are presented for the first time. It was established that waters under study are supersaturated with respect to calcite and siderite, and to a smaller extent with respect to magnesite and dolomite. No saturation of radon waters with respect to primary aluminosilicate minerals (albite, anortite, microcline, ferrosilite) is observed. The points are located in the fields of stability of clayey minerals (kaolinite, Ca- and Mg-montmorillonite, Fe-sepiolite), gibbsite and leptochlorite. In the evolution of the water-rock system, they correspond to the siallite type of interaction with rocks.

AB - Results of thermodynamic calculations of the interactions of radon waters from the Zaeltsovsky field with the minerals of host rocks are presented for the first time. It was established that waters under study are supersaturated with respect to calcite and siderite, and to a smaller extent with respect to magnesite and dolomite. No saturation of radon waters with respect to primary aluminosilicate minerals (albite, anortite, microcline, ferrosilite) is observed. The points are located in the fields of stability of clayey minerals (kaolinite, Ca- and Mg-montmorillonite, Fe-sepiolite), gibbsite and leptochlorite. In the evolution of the water-rock system, they correspond to the siallite type of interaction with rocks.

KW - equilibrium

KW - hydrogeochemistry

KW - Novosibirsk

KW - radon waters

KW - water-rock system

KW - Western Siberia

UR - http://www.scopus.com/inward/record.url?scp=85091736905&partnerID=8YFLogxK

U2 - 10.1088/1742-6596/1451/1/012007

DO - 10.1088/1742-6596/1451/1/012007

M3 - Conference article

AN - SCOPUS:85091736905

VL - 1451

JO - Journal of Physics: Conference Series

JF - Journal of Physics: Conference Series

SN - 1742-6588

IS - 1

M1 - 012007

T2 - 2nd International Conference on Applied Physics, Power and Material Science, ICAPPM 2019

Y2 - 20 December 2019 through 21 December 2019

ER -

ID: 25613652