Mechanisms of Accumulation of Chemical Elements in a Peat Deposit in the Eastern Part of Vasyugan Swamp (West Siberia); Doklady Earth Sciences; Vol. 486, iss. 1

Bibliografiset tiedot
Parent link:Doklady Earth Sciences
Vol. 486, iss. 1.— 2019.— [P. 568-570]
Yhteisötekijät: Национальный исследовательский Томский политехнический университет Инженерная школа природных ресурсов Отделение геологии, Национальный исследовательский Томский политехнический университет Институт природных ресурсов Кафедра геологии и разведки полезных ископаемых Международная научно-образовательная лаборатория изучения углерода арктических морей
Muut tekijät: Savichev O. G. Oleg Gennadievich, Mazurov A. K. Aleksey Karpovich, Rudmin M. A. Maksim Andreevich, Shakhova N. E. Nataljya Evgenjevna, Sergienko V. I. Valentin, Semiletov I. P. Igor Petrovich
Yhteenveto:Title screen
The results of mineralogical-geochemical studies of the oligotrophic pine-fruticulose-sphagnum segment of Vasyugan Swamp (West Siberia) in the winter of 2017 are presented. A mathematical model is developed for the depth distribution of chemical elements in water and acid extracts of peats, organo-mineral sediments, and inorganic soil. It is shown that two complex geochemical barriers related to the changes in filtration properties of soils and contributing to the formation and/or accumulation of Fe compounds and other chemical elements function in the peat deposit. The first (oxidizing, reduction, sulfide, and adsorption hydroxide) barrier is found approximately at a depth of 0.40-1.25 m; the second (alkaline carbonate and hydrolytic, adsorption hydroxide, clayey, and carbonate) barrier lies in the lower layer of the peat deposit (a depth of 2.25-2.50 m). The result obtained is important for understanding the production-destruction methane cycle.
Режим доступа: по договору с организацией-держателем ресурса
Kieli:englanti
Julkaistu: 2019
Aiheet:
Linkit:https://doi.org/10.1134/S1028334X19050258
Aineistotyyppi: Elektroninen Kirjan osa
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=660742

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200 1 |a Mechanisms of Accumulation of Chemical Elements in a Peat Deposit in the Eastern Part of Vasyugan Swamp (West Siberia)  |f O. G. Savichev [et al.] 
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330 |a The results of mineralogical-geochemical studies of the oligotrophic pine-fruticulose-sphagnum segment of Vasyugan Swamp (West Siberia) in the winter of 2017 are presented. A mathematical model is developed for the depth distribution of chemical elements in water and acid extracts of peats, organo-mineral sediments, and inorganic soil. It is shown that two complex geochemical barriers related to the changes in filtration properties of soils and contributing to the formation and/or accumulation of Fe compounds and other chemical elements function in the peat deposit. The first (oxidizing, reduction, sulfide, and adsorption hydroxide) barrier is found approximately at a depth of 0.40-1.25 m; the second (alkaline carbonate and hydrolytic, adsorption hydroxide, clayey, and carbonate) barrier lies in the lower layer of the peat deposit (a depth of 2.25-2.50 m). The result obtained is important for understanding the production-destruction methane cycle. 
333 |a Режим доступа: по договору с организацией-держателем ресурса 
461 |t Doklady Earth Sciences 
463 |t Vol. 486, iss. 1  |v [P. 568-570]  |d 2019 
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