Standard

Hydrogeochemistry and stable isotopes in radon-rich thermal waters of Belokurikha (Altai, Russia). / Novikov, Dmitry A.; Khvaschevskaya, Albina A.; Kopylova, Yulia G. и др.

в: Environmental Science and Pollution Research, Том 29, № 55, 11.2022, стр. 83081-83098.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Novikov, DA, Khvaschevskaya, AA, Kopylova, YG, Pyryaev, AN, Maksimova, AA, Derkachev, AS, Dultsev, FF, Chernykh, AV & Purgina, DV 2022, 'Hydrogeochemistry and stable isotopes in radon-rich thermal waters of Belokurikha (Altai, Russia)', Environmental Science and Pollution Research, Том. 29, № 55, стр. 83081-83098. https://doi.org/10.1007/s11356-022-21640-w

APA

Novikov, D. A., Khvaschevskaya, A. A., Kopylova, Y. G., Pyryaev, A. N., Maksimova, A. A., Derkachev, A. S., Dultsev, F. F., Chernykh, A. V., & Purgina, D. V. (2022). Hydrogeochemistry and stable isotopes in radon-rich thermal waters of Belokurikha (Altai, Russia). Environmental Science and Pollution Research, 29(55), 83081-83098. https://doi.org/10.1007/s11356-022-21640-w

Vancouver

Novikov DA, Khvaschevskaya AA, Kopylova YG, Pyryaev AN, Maksimova AA, Derkachev AS и др. Hydrogeochemistry and stable isotopes in radon-rich thermal waters of Belokurikha (Altai, Russia). Environmental Science and Pollution Research. 2022 нояб.;29(55):83081-83098. Epub 2022 июнь 27. doi: 10.1007/s11356-022-21640-w

Author

Novikov, Dmitry A. ; Khvaschevskaya, Albina A. ; Kopylova, Yulia G. и др. / Hydrogeochemistry and stable isotopes in radon-rich thermal waters of Belokurikha (Altai, Russia). в: Environmental Science and Pollution Research. 2022 ; Том 29, № 55. стр. 83081-83098.

BibTeX

@article{d92eb7fc360e4f5da0e070a439bcf4e7,
title = "Hydrogeochemistry and stable isotopes in radon-rich thermal waters of Belokurikha (Altai, Russia)",
abstract = "The first integrated isotope and chemistry results have been obtained for radon-rich thermal waters from the Belokurikha field which are used at a large spa resort in Altai, Russia. The waters reside in an unconfined aquifer composed of Quaternary soft sediments and in a confined (artesian) aquifer of monolithic to weathered Upper Paleozoic granites. The waters belong to three geochemical groups: low-radon nitrogen-silicic interstitial waters in weathered Paleozoic granites; groundwaters of REE-enriched and background compositions; surface waters of the Belokurikha River. The interstitial waters in granites have HCO3-SO4 Na and SO4-HCO3 Na major-ion chemistry, total salinity from 198 to 257 mg/L, pH = 8.6–9.6, silica contents of 19.8 to 24.6 mg/L, and 222Rn activity from 160 to 360 Bq/L (290 Bq/L on average). Judging by their oxygen and hydrogen (deuterium) isotope compositions (−17.5 to −14.2 ‰ and −126.9 to −102.7 ‰, respectively), the Belokurikha aquifers recharge with infiltrating meteoric water, especially the winter precipitation. The carbon isotope composition of dissolved inorganic carbon (−9.7 to −25.6 ‰ δ13СDIC) corresponds to biogenic origin. Comparison of radon-rich mineral waters from different areas of southern Siberia shows that the change from oxidized to reduced environments leads to 232Th/238U increase from 4.20∙10−5–7.39∙10−2 to 0.0022–26, respectively, with an intermediate range of 2.63∙10−5–0.20 in transitional conditions.",
keywords = "Ra, Th, U, Belokurikha spa, Stable isotopes, Thermal water, Environmental Monitoring, Oxygen Isotopes/analysis, Salinity, Groundwater/chemistry, Radon/analysis, Mineral Waters, Isotopes, 238U, 222Ra, 232Th",
author = "Novikov, {Dmitry A.} and Khvaschevskaya, {Albina A.} and Kopylova, {Yulia G.} and Pyryaev, {Aleksandr N.} and Maksimova, {Anastasia A.} and Derkachev, {Anton S.} and Dultsev, {Fedor F.} and Chernykh, {Anatoliy V.} and Purgina, {Daria V.}",
note = "Funding Information: The work was supported by the Ministry of Science and Education of the Russian Federation under Projects No. FWZZ-2022-0014 and No.FSWW-0022-2020. Publisher Copyright: {\textcopyright} 2022, The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature.",
year = "2022",
month = nov,
doi = "10.1007/s11356-022-21640-w",
language = "English",
volume = "29",
pages = "83081--83098",
journal = "Environmental Science and Pollution Research",
issn = "0944-1344",
publisher = "Springer Science + Business Media",
number = "55",

}

RIS

TY - JOUR

T1 - Hydrogeochemistry and stable isotopes in radon-rich thermal waters of Belokurikha (Altai, Russia)

AU - Novikov, Dmitry A.

AU - Khvaschevskaya, Albina A.

AU - Kopylova, Yulia G.

AU - Pyryaev, Aleksandr N.

AU - Maksimova, Anastasia A.

AU - Derkachev, Anton S.

AU - Dultsev, Fedor F.

AU - Chernykh, Anatoliy V.

AU - Purgina, Daria V.

N1 - Funding Information: The work was supported by the Ministry of Science and Education of the Russian Federation under Projects No. FWZZ-2022-0014 and No.FSWW-0022-2020. Publisher Copyright: © 2022, The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature.

PY - 2022/11

Y1 - 2022/11

N2 - The first integrated isotope and chemistry results have been obtained for radon-rich thermal waters from the Belokurikha field which are used at a large spa resort in Altai, Russia. The waters reside in an unconfined aquifer composed of Quaternary soft sediments and in a confined (artesian) aquifer of monolithic to weathered Upper Paleozoic granites. The waters belong to three geochemical groups: low-radon nitrogen-silicic interstitial waters in weathered Paleozoic granites; groundwaters of REE-enriched and background compositions; surface waters of the Belokurikha River. The interstitial waters in granites have HCO3-SO4 Na and SO4-HCO3 Na major-ion chemistry, total salinity from 198 to 257 mg/L, pH = 8.6–9.6, silica contents of 19.8 to 24.6 mg/L, and 222Rn activity from 160 to 360 Bq/L (290 Bq/L on average). Judging by their oxygen and hydrogen (deuterium) isotope compositions (−17.5 to −14.2 ‰ and −126.9 to −102.7 ‰, respectively), the Belokurikha aquifers recharge with infiltrating meteoric water, especially the winter precipitation. The carbon isotope composition of dissolved inorganic carbon (−9.7 to −25.6 ‰ δ13СDIC) corresponds to biogenic origin. Comparison of radon-rich mineral waters from different areas of southern Siberia shows that the change from oxidized to reduced environments leads to 232Th/238U increase from 4.20∙10−5–7.39∙10−2 to 0.0022–26, respectively, with an intermediate range of 2.63∙10−5–0.20 in transitional conditions.

AB - The first integrated isotope and chemistry results have been obtained for radon-rich thermal waters from the Belokurikha field which are used at a large spa resort in Altai, Russia. The waters reside in an unconfined aquifer composed of Quaternary soft sediments and in a confined (artesian) aquifer of monolithic to weathered Upper Paleozoic granites. The waters belong to three geochemical groups: low-radon nitrogen-silicic interstitial waters in weathered Paleozoic granites; groundwaters of REE-enriched and background compositions; surface waters of the Belokurikha River. The interstitial waters in granites have HCO3-SO4 Na and SO4-HCO3 Na major-ion chemistry, total salinity from 198 to 257 mg/L, pH = 8.6–9.6, silica contents of 19.8 to 24.6 mg/L, and 222Rn activity from 160 to 360 Bq/L (290 Bq/L on average). Judging by their oxygen and hydrogen (deuterium) isotope compositions (−17.5 to −14.2 ‰ and −126.9 to −102.7 ‰, respectively), the Belokurikha aquifers recharge with infiltrating meteoric water, especially the winter precipitation. The carbon isotope composition of dissolved inorganic carbon (−9.7 to −25.6 ‰ δ13СDIC) corresponds to biogenic origin. Comparison of radon-rich mineral waters from different areas of southern Siberia shows that the change from oxidized to reduced environments leads to 232Th/238U increase from 4.20∙10−5–7.39∙10−2 to 0.0022–26, respectively, with an intermediate range of 2.63∙10−5–0.20 in transitional conditions.

KW - Ra

KW - Th

KW - U

KW - Belokurikha spa

KW - Stable isotopes

KW - Thermal water

KW - Environmental Monitoring

KW - Oxygen Isotopes/analysis

KW - Salinity

KW - Groundwater/chemistry

KW - Radon/analysis

KW - Mineral Waters

KW - Isotopes

KW - 238U

KW - 222Ra

KW - 232Th

UR - http://www.scopus.com/inward/record.url?scp=85132797136&partnerID=8YFLogxK

UR - https://www.mendeley.com/catalogue/77579577-eccc-3f80-bc66-d389837918a3/

U2 - 10.1007/s11356-022-21640-w

DO - 10.1007/s11356-022-21640-w

M3 - Article

C2 - 35761131

AN - SCOPUS:85132797136

VL - 29

SP - 83081

EP - 83098

JO - Environmental Science and Pollution Research

JF - Environmental Science and Pollution Research

SN - 0944-1344

IS - 55

ER -

ID: 36497258