Soda groundwater of the southern part of Kuzbass (Russia); SGEM. 17th International Multidisciplinary Scientific GeoConferences; Vol. 16, iss. 12
| Parent link: | SGEM. 17th International Multidisciplinary Scientific GeoConferences: conference proceedings, Albena, Bulgariaм, 29 June-5 July 2017 Vol. 16, iss. 12.— 2017.— [P. 735-742] |
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| 要約: | Title screen Conditions of manifestation, feature of chemical and isotope composition of soda groundwater of the southern part of Kuzbass - the world's largest coal basin have been studied. It is shown that soda groundwater is widely developed here within of coal-bearing sand-clay of Paleozoic sediments, are confined in zone of slow water exchange at depths from 100-200 up to 2000 m. At the same time soda groundwater are presented quite variously on chemical and isotope compositions, that has allowed to allocate them in three groups: 1) soda groundwater with a low mineralization (0.2-5 g/l) of the upper part of zone of slow water exchange (at depths of about 100-1000 m) with values δD from -125.6 ‰ to -101.8 ‰, δ18O: from -17.7 ‰ to -15.0 ‰ and δ13C from -12.4 ‰ to -6.7; 2) soda groundwater with a high mineralization (up to 25 g/l) of the lower part of zone of slow water exchange (at depths of about 400-2000 m), which enriched 18O (δ18O from -14.9 ‰ to -11.9 ‰) and 13C (δ13С from +4.7 to +30.9‰); 3) soda groundwater with СО2 of mixed genesis (δ13С from -12.3 to -3.9 ‰) (in certain points). It was determined, that three groups have infiltration origin and first both groups have biogenic source of carbonic acid. Режим доступа: по договору с организацией-держателем ресурса |
| 言語: | 英語 |
| 出版事項: |
2017
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| シリーズ: | Hydrogeology, Engineering Geology and Geotechnics |
| 主題: | |
| オンライン･アクセス: | https://www.elibrary.ru/item.asp?id=42655814 |
| フォーマット: | MixedMaterials 電子媒体 図書の章 |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=666696 |
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| 200 | 1 | |a Soda groundwater of the southern part of Kuzbass (Russia) |f О. Е. Lepokurova | |
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| 225 | 1 | |a Hydrogeology, Engineering Geology and Geotechnics | |
| 300 | |a Title screen | ||
| 330 | |a Conditions of manifestation, feature of chemical and isotope composition of soda groundwater of the southern part of Kuzbass - the world's largest coal basin have been studied. It is shown that soda groundwater is widely developed here within of coal-bearing sand-clay of Paleozoic sediments, are confined in zone of slow water exchange at depths from 100-200 up to 2000 m. At the same time soda groundwater are presented quite variously on chemical and isotope compositions, that has allowed to allocate them in three groups: 1) soda groundwater with a low mineralization (0.2-5 g/l) of the upper part of zone of slow water exchange (at depths of about 100-1000 m) with values δD from -125.6 ‰ to -101.8 ‰, δ18O: from -17.7 ‰ to -15.0 ‰ and δ13C from -12.4 ‰ to -6.7; 2) soda groundwater with a high mineralization (up to 25 g/l) of the lower part of zone of slow water exchange (at depths of about 400-2000 m), which enriched 18O (δ18O from -14.9 ‰ to -11.9 ‰) and 13C (δ13С from +4.7 to +30.9‰); 3) soda groundwater with СО2 of mixed genesis (δ13С from -12.3 to -3.9 ‰) (in certain points). It was determined, that three groups have infiltration origin and first both groups have biogenic source of carbonic acid. | ||
| 333 | |a Режим доступа: по договору с организацией-держателем ресурса | ||
| 461 | |t SGEM. 17th International Multidisciplinary Scientific GeoConferences |o conference proceedings, Albena, Bulgariaм, 29 June-5 July 2017 | ||
| 463 | |t Vol. 16, iss. 12 |v [P. 735-742] |d 2017 | ||
| 610 | 1 | |a электронный ресурс | |
| 610 | 1 | |a труды учёных ТПУ | |
| 610 | 1 | |a soda groundwater | |
| 610 | 1 | |a coal deposits | |
| 610 | 1 | |a chemical and isotopic composition | |
| 610 | 1 | |a Kuzbass | |
| 610 | 1 | |a содовые воды | |
| 610 | 1 | |a подземные воды | |
| 610 | 1 | |a угольные месторождения | |
| 610 | 1 | |a химический состав | |
| 610 | 1 | |a изотопный состав | |
| 610 | 1 | |a Кузбасс | |
| 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 | |
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