S.V. Rasskazov1,2, E.P. Chebykin1,3, I.S. Chuvashova1,2, A.M. Ilyasova1, S.V. Snopkov2,4, Yi-min Sun5
1Institute of the Earth's Crust SB RAS, Irkutsk, Russia
2Irkutsk State University, Irkutsk, Russia
3Limnological Institute SB RAS, Irkutsk, Russia
4Siberian School of Geosciences, Irkutsk National Research Technical University, Irkutsk, Russia
5Institute of Natural Resources and Ecology, Heilongjiang Academy of Sciences, Harbin, China
Rasskazov Sergei Vasilievich,
doctor of geological and mineralogical sciences, professor,
664025, Irkutsk, Lenin st., 3,
Irkutsk State University, Faculty of Geology,
Head of Dynamic Geology Char,
664033, Irkutsk, Lermontov st., 128,
Institute of the Earth's Crust SB RAS,
Head of Laboratory for Isotopic and Geochronological Studies,
tel.: (3952) 51–16–59,
email: rassk@crust.irk.ru.
Chebykin Evgeny Pavlovich,
Candidate of Chemical Sciences, Senior Researcher,
664033, Irkutsk, st. Lermontova, d. 128,
Institute of the Earth's Crust SB RAS
664033, Irkutsk, st. Ulan-Batorskaya, 3,
Limnological Institute SB RAS,
email: epcheb@yandex.ru.
Chuvashova Irina Sergeevna,
candidate of geological and mineralogical sciences,
664025, Irkutsk, Lenin st., 3,
Irkutsk State University, Faculty of Geology,
Associate Professor of the Dynamic Geology chair,
664033, Irkutsk, Lermontov st., 128,
Institute of the Earth's Crust SB RAS,
Senior Researcher,
tel.: (3952) 51–16–59,
email: chuvashova@crust.irk.ru.
Ilyasova Aigul Maratovna,
candidate of geological and mineralogical sciences,
664033, Irkutsk, st. Lermontova, d. 128,
Institute of the Earth's Crust SB RAS,
leading engineer,
email: ila@crust.irk.ru.
Snopkov Sergey Viktorovich,
Candidate of Geological and Mineralogical Sciences, assistant professor,
664025, Irkutsk, st. Lenina, 3,
Irkutsk State University, Faculty of Geology,
664074, Irkutsk, st. Kurchatova, 3,
Siberian School of Geosciences, Irkutsk National Research Technical University,
Leading Researcher
email: snopkov_serg@mail.ru.
Yi-min Sun,
Institute of Natural Resources and Ecology, Heilongjiang Academy of Sciences, Harbin, China,
Researcher,
email: 894817259@qq.com.
Abstract. Monitoring series of the 234U/238U activity ratio, concentrations of U, and Si – Na/Li temperatures in reservoir of groundwater from the Arshan sanatorium area in the Tunka Valley are obtained in 2012–2024. With taking into account published materials and existing ideas on the groundwater genesis in the Tunka Valley, it is proposed that the entry of uranium components into groundwater is controlled by uranium dissolution under the influence of gases – oxidizers and reducers. It is augured that the isotopic equilibrium between 234U and 238 in cold carbon dioxide mineral waters can serve as an indicator of the impact of oxidized fluids on their deep reservoir, and the disruption of the equilibrium can serve as an indicator of the replacement of the affecting oxidized fluids by reduced ones. The monitoring data series are used to trace paragenetic relationship between hydrogeochemical, seismic, and volcanic processes in the Baikal Rift System.
Keywords: Baikal, Tunka Valley, groundwater, 234U/238U, Cherdyntsev–Chalov effect, earthquakes.
P. 65–112
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