Geochemistry of soda waters of the Chulym–Yenisei Artesian Basin (West Siberia); Russian Geology and Geophysics; Vol. 60, iss. 5
| Parent link: | Russian Geology and Geophysics Vol. 60, iss. 5.— 2019.— [P. 558-569] |
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| Summary: | Title screen Results of studies of soda waters of the Chulym–Yenisei artesian basin are presented. It is shown that these waters are ubiquitous within Cretaceous or Jurassic sediments at depths of ~100–300 m to 1.5–2.3 km. According to the formation conditions, mineralization, and pH, they are divided into three groups: Type I waters spread to a depth of 600 m and have pH = 7.4–8.4 and TDS ? 0.5 g/L, type II soda waters occur at depths of 0.6–2.3 km and are characterized by pH = 8.0–8.9 and TDS = 0.7–4.1 g/L, and type III waters («Omega») form a local segment among type II waters and have a unique composition: high alkalinity (pH = 9.0–10.3) and low mineralization (TSD = 0.2–0.6 g/L). We focus special attention on type III waters and present results of studies of their microcomponent, gas, and isotope compositions. The cause of their low salinity and high pH is explained for the first time. Taking into account the isotope data (?D, ?18O, and ?13C), we have established the infiltration origin of soda waters of the three types and the biogenic source of their carbon dioxide. Calculations of equilibria in the water–host-mineral system have shown that all soda waters are in disequilibrium with many primary alu-minosilicate minerals but are in equilibrium with a wide range of carbonates and clays. In passing from type I to type III waters, the number of minerals in equilibrium with water continuously increases (albite, microcline, muscovite, and biotite). Taking into account the data obtained, we present schemes of formation of different types of soda waters in the studied basin at different stages of the evolution of the water–rock–gas–organic-matter sys-tem and estimate the time of each system. Режим доступа: по договору с организацией-держателем ресурса |
| Language: | English |
| Published: |
2019
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| Subjects: | |
| Online Access: | https://doi.org/10.15372/RGG2019044 |
| Format: | Electronic Book Chapter |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=662391 |
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| 200 | 1 | |a Geochemistry of soda waters of the Chulym–Yenisei Artesian Basin (West Siberia) |f О. Е. Lepokurova, S. L. Shvartsev | |
| 203 | |a Text |c electronic | ||
| 300 | |a Title screen | ||
| 330 | |a Results of studies of soda waters of the Chulym–Yenisei artesian basin are presented. It is shown that these waters are ubiquitous within Cretaceous or Jurassic sediments at depths of ~100–300 m to 1.5–2.3 km. According to the formation conditions, mineralization, and pH, they are divided into three groups: Type I waters spread to a depth of 600 m and have pH = 7.4–8.4 and TDS ? 0.5 g/L, type II soda waters occur at depths of 0.6–2.3 km and are characterized by pH = 8.0–8.9 and TDS = 0.7–4.1 g/L, and type III waters («Omega») form a local segment among type II waters and have a unique composition: high alkalinity (pH = 9.0–10.3) and low mineralization (TSD = 0.2–0.6 g/L). We focus special attention on type III waters and present results of studies of their microcomponent, gas, and isotope compositions. The cause of their low salinity and high pH is explained for the first time. Taking into account the isotope data (?D, ?18O, and ?13C), we have established the infiltration origin of soda waters of the three types and the biogenic source of their carbon dioxide. Calculations of equilibria in the water–host-mineral system have shown that all soda waters are in disequilibrium with many primary alu-minosilicate minerals but are in equilibrium with a wide range of carbonates and clays. In passing from type I to type III waters, the number of minerals in equilibrium with water continuously increases (albite, microcline, muscovite, and biotite). Taking into account the data obtained, we present schemes of formation of different types of soda waters in the studied basin at different stages of the evolution of the water–rock–gas–organic-matter sys-tem and estimate the time of each system. | ||
| 333 | |a Режим доступа: по договору с организацией-держателем ресурса | ||
| 461 | |t Russian Geology and Geophysics | ||
| 463 | |t Vol. 60, iss. 5 |v [P. 558-569] |d 2019 | ||
| 610 | 1 | |a электронный ресурс | |
| 610 | 1 | |a труды учёных ТПУ | |
| 610 | 1 | |a soda waters | |
| 610 | 1 | |a conditions of water spread | |
| 610 | 1 | |a chemical and isotope compositions | |
| 610 | 1 | |a water–rock system | |
| 610 | 1 | |a for-mation mechanisms | |
| 610 | 1 | |a equilibrium | |
| 610 | 1 | |a Chulym–Yenisei basin | |
| 610 | 1 | |a содовые воды | |
| 610 | 1 | |a химический состав | |
| 610 | 1 | |a изотопный состав | |
| 610 | 1 | |a Чулымский бассейн | |
| 700 | 1 | |a Lepokurova |b О. Е. |c geologist |c Professor of Tomsk Polytechnic University, Doctor of Geological and Mineralogical Sciences |f 1980- |g Olesya Evgenyevna |3 (RuTPU)RU\TPU\pers\32568 |9 16489 | |
| 701 | 1 | |a Shvartsev |b S. L. |c Russian hydrogeologist, Doctor of Geological and Mineralogical sciences |c Professor of the TPU, Member of the Academy of Natural sciences |f 1936-2018 |g Stepan Lvovich |3 (RuTPU)RU\TPU\pers\24144 |9 10674 | |
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