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DISTRIBUTION OF REE AND U IN THE WATER-ROCK SYSTEM USING THE EXAMPLE OF THE SKALINSKOYE MANIFESTATION OF RADON WATERS. / Novikov, D. A.; Maksimova, A. A.; Sukhorukova, A. F. et al.

In: Geology and Mineral Resources of Siberia, No. 3, 2024, p. 141-151.

Research output: Contribution to journal › Article › peer-review

Harvard

Novikov, DA, Maksimova, AA, Sukhorukova, AF, Dultsev, FF, Derkachev, AS, Chernykh, AV & Khvashchevskaya, AA 2024, 'DISTRIBUTION OF REE AND U IN THE WATER-ROCK SYSTEM USING THE EXAMPLE OF THE SKALINSKOYE MANIFESTATION OF RADON WATERS', Geology and Mineral Resources of Siberia, no. 3, pp. 141-151. https://doi.org/10.20403/2078-0575-2024-3-141-151

APA

Novikov, D. A., Maksimova, A. A., Sukhorukova, A. F., Dultsev, F. F., Derkachev, A. S., Chernykh, A. V., & Khvashchevskaya, A. A. (2024). DISTRIBUTION OF REE AND U IN THE WATER-ROCK SYSTEM USING THE EXAMPLE OF THE SKALINSKOYE MANIFESTATION OF RADON WATERS. Geology and Mineral Resources of Siberia, (3), 141-151. https://doi.org/10.20403/2078-0575-2024-3-141-151

Vancouver

Novikov DA, Maksimova AA, Sukhorukova AF, Dultsev FF, Derkachev AS, Chernykh AV et al. DISTRIBUTION OF REE AND U IN THE WATER-ROCK SYSTEM USING THE EXAMPLE OF THE SKALINSKOYE MANIFESTATION OF RADON WATERS. Geology and Mineral Resources of Siberia. 2024;(3):141-151. doi: 10.20403/2078-0575-2024-3-141-151

Author

Novikov, D. A. ; Maksimova, A. A. ; Sukhorukova, A. F. et al. / DISTRIBUTION OF REE AND U IN THE WATER-ROCK SYSTEM USING THE EXAMPLE OF THE SKALINSKOYE MANIFESTATION OF RADON WATERS. In: Geology and Mineral Resources of Siberia. 2024 ; No. 3. pp. 141-151.

BibTeX

@article{ddc4a9db649b4033a29e69a1f9574efb,
title = "DISTRIBUTION OF REE AND U IN THE WATER-ROCK SYSTEM USING THE EXAMPLE OF THE SKALINSKOYE MANIFESTATION OF RADON WATERS",
abstract = "The paper presents data on geochemical features of the water-rock system of the Skalinskoye radon water manifestation. The waters of the Skalinskoye manifestation by chemical composition belong to the SO4-HCO3 Na-Mg-Ca type with a total mineralization value of 279–787 mg/dm3. The geochemical parameters of the medium correspond to the oxidizing environment with Eh +84,6…+187,0 mV, pH 6.9–8.8 and O2dissolved concentrations of 3.75–9.93 mg/dm3. Radon activity is up to 572 Bq/dm3. The water-bearing rocks are represented by biotite granites of normal and moderately alkaline series, which are permeated by quartz and sericite-quartz veins. With an increase in the total mineralization of radon waters, the prevailing forms of migration are calcium, magnesium, nickel and strontium bicarbonates, nickel carbonate and magnesium sulfate. Uranium migrates mainly in the form of dissolved hydroxide U(OH)4(aq). According to saturation indices, all waters are saturated in relation to calcite, uraninite and amorphous uranium oxide.",
keywords = "REE, West Siberia, granites, migration forms, new manifestation of radon waters Skalinskoye, radionuclides, radon waters",
author = "Novikov, {D. A.} and Maksimova, {A. A.} and Sukhorukova, {A. F.} and Dultsev, {F. F.} and Derkachev, {A. S.} and Chernykh, {A. V.} and Khvashchevskaya, {A. A.}",
year = "2024",
doi = "10.20403/2078-0575-2024-3-141-151",
language = "русский",
pages = "141--151",
journal = "Геология и минерально-сырьевые ресурсы Сибири",
issn = "2078-0575",
publisher = "Федеральное государственное унитарное предприятие Сибирский научно-исследовательский институт геологии, геофизики и минерального сырья",
number = "3",

}

RIS

TY - JOUR

T1 - DISTRIBUTION OF REE AND U IN THE WATER-ROCK SYSTEM USING THE EXAMPLE OF THE SKALINSKOYE MANIFESTATION OF RADON WATERS

AU - Novikov, D. A.

AU - Maksimova, A. A.

AU - Sukhorukova, A. F.

AU - Dultsev, F. F.

AU - Derkachev, A. S.

AU - Chernykh, A. V.

AU - Khvashchevskaya, A. A.

PY - 2024

Y1 - 2024

N2 - The paper presents data on geochemical features of the water-rock system of the Skalinskoye radon water manifestation. The waters of the Skalinskoye manifestation by chemical composition belong to the SO4-HCO3 Na-Mg-Ca type with a total mineralization value of 279–787 mg/dm3. The geochemical parameters of the medium correspond to the oxidizing environment with Eh +84,6…+187,0 mV, pH 6.9–8.8 and O2dissolved concentrations of 3.75–9.93 mg/dm3. Radon activity is up to 572 Bq/dm3. The water-bearing rocks are represented by biotite granites of normal and moderately alkaline series, which are permeated by quartz and sericite-quartz veins. With an increase in the total mineralization of radon waters, the prevailing forms of migration are calcium, magnesium, nickel and strontium bicarbonates, nickel carbonate and magnesium sulfate. Uranium migrates mainly in the form of dissolved hydroxide U(OH)4(aq). According to saturation indices, all waters are saturated in relation to calcite, uraninite and amorphous uranium oxide.

AB - The paper presents data on geochemical features of the water-rock system of the Skalinskoye radon water manifestation. The waters of the Skalinskoye manifestation by chemical composition belong to the SO4-HCO3 Na-Mg-Ca type with a total mineralization value of 279–787 mg/dm3. The geochemical parameters of the medium correspond to the oxidizing environment with Eh +84,6…+187,0 mV, pH 6.9–8.8 and O2dissolved concentrations of 3.75–9.93 mg/dm3. Radon activity is up to 572 Bq/dm3. The water-bearing rocks are represented by biotite granites of normal and moderately alkaline series, which are permeated by quartz and sericite-quartz veins. With an increase in the total mineralization of radon waters, the prevailing forms of migration are calcium, magnesium, nickel and strontium bicarbonates, nickel carbonate and magnesium sulfate. Uranium migrates mainly in the form of dissolved hydroxide U(OH)4(aq). According to saturation indices, all waters are saturated in relation to calcite, uraninite and amorphous uranium oxide.

KW - REE

KW - West Siberia

KW - granites

KW - migration forms

KW - new manifestation of radon waters Skalinskoye

KW - radionuclides

KW - radon waters

UR - https://www.scopus.com/record/display.uri?eid=2-s2.0-85210291524&origin=inward&txGid=6bea4b7746a006f415e14b02e0c9be09

UR - https://www.mendeley.com/catalogue/d4f42377-46d3-3409-a707-1ea3f0e5c4da/

U2 - 10.20403/2078-0575-2024-3-141-151

DO - 10.20403/2078-0575-2024-3-141-151

M3 - статья

SP - 141

EP - 151

JO - Геология и минерально-сырьевые ресурсы Сибири

JF - Геология и минерально-сырьевые ресурсы Сибири

SN - 2078-0575

IS - 3

ER -

ID: 61301130