Mineralogical and Geochemical Features of a Peat Deposit in the Eutrophic Obskoye Fen under Anthropogenic Load (Western Siberia); Doklady Earth Sciences; Vol. 492, iss. 1

Бібліографічні деталі
Parent link:Doklady Earth Sciences
Vol. 492, iss. 1.— 2020.— [P. 320-322]
Співавтор: Национальный исследовательский Томский политехнический университет Инженерная школа природных ресурсов Отделение геологии
Інші автори: Savichev O. G. Oleg Gennadievich, Rudmin M. A. Maksim Andreevich, Mazurov A. K. Aleksey Karpovich, Nalivayko N. G. Nina Grigorievna, Sergienko V. I. Valentin, Semiletov I. P. Igor Petrovich
Резюме:Title screen
The chemical composition and mineral inclusions in peats and the underlying soils of the eutrophic Obskoye fen (Western Siberia, Tomsk Region) are studied. The basic pattern of a change in the mineralogical and geochemical conditions at depth consists in domination of hydroxides on top of the peat deposit and sulfides at the bottom. The geochemical reduction barrier is formed at the bottom of the peat deposit. Its functioning is related to increased concentrations of U and Hg. The markedly pronounced influence exerted by sewage discharge is associated with an increase in the Na concentration in acid extracts from peats and additional accumulation of the mixture of suspended, colloidal, and dissolved forms of some metals in the boggy environment.
Режим доступа: по договору с организацией-держателем ресурса
Мова:Англійська
Опубліковано: 2020
Предмети:
Онлайн доступ:https://doi.org/10.1134/S1028334X20050219
Формат: Електронний ресурс Частина з книги
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=663509

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200 1 |a Mineralogical and Geochemical Features of a Peat Deposit in the Eutrophic Obskoye Fen under Anthropogenic Load (Western Siberia)  |d Минералого-геохимические особенности торфяной залежи эвтрофного Обского болота в условиях антропогенной нагрузки (Западная Сибирь)  |f O. G. Savichev, M. A. Rudmin, A. K. Mazurov [et al.] 
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330 |a The chemical composition and mineral inclusions in peats and the underlying soils of the eutrophic Obskoye fen (Western Siberia, Tomsk Region) are studied. The basic pattern of a change in the mineralogical and geochemical conditions at depth consists in domination of hydroxides on top of the peat deposit and sulfides at the bottom. The geochemical reduction barrier is formed at the bottom of the peat deposit. Its functioning is related to increased concentrations of U and Hg. The markedly pronounced influence exerted by sewage discharge is associated with an increase in the Na concentration in acid extracts from peats and additional accumulation of the mixture of suspended, colloidal, and dissolved forms of some metals in the boggy environment. 
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461 |t Doklady Earth Sciences 
463 |t Vol. 492, iss. 1  |v [P. 320-322]  |d 2020 
510 1 |a Минералого-геохимические особенности торфяной залежи эвтрофного Обского болота в условиях антропогенной нагрузки (Западная Сибирь)  |z rus 
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610 1 |a Western Siberia 
701 1 |a Savichev  |b O. G.  |c geologist  |c Professor of Tomsk Polytechnic University, doctor of geographical sciences  |f 1967-  |g Oleg Gennadievich  |3 (RuTPU)RU\TPU\pers\34024  |9 17591 
701 1 |a Rudmin  |b M. A.  |c geologist  |c Associate Professor of Tomsk Polytechnic University, Candidate of Geological and Mineralogical Sciences  |f 1989-  |g Maksim Andreevich  |3 (RuTPU)RU\TPU\pers\33254  |9 16999 
701 1 |a Mazurov  |b A. K.  |c geologist  |c Professor-consultant of Tomsk Polytechnic University, Doctor of Geological and Mineralogical Sciences  |f 1951-  |g Aleksey Karpovich   |3 (RuTPU)RU\TPU\pers\30165  |9 14563 
701 1 |a Nalivayko  |b N. G.  |c hydrogeologist  |c Associate Professor of Tomsk Polytechnic University, Candidate of geological and mineralogical sciences  |f 1946-  |g Nina Grigorievna  |3 (RuTPU)RU\TPU\pers\33258  |9 17003 
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