Water-rock interaction within the oligotrophic peat bog (part of the Vasyugan Swamp, Western Siberia)

Аннотация

Geochemical conditions of the formation of various minerals were studied within the oligotrophic pine-shrub and sphagnum peat bog. It was shown that at least two complex barriers function within the peat deposit. These barriers correspond to the changes in the advective and diffusion transfer of substances and promote the immobilization of Fe and a number of other chemical elements. The upper complex geochemical (redox, sulfide and sorption) barrier occurs approximately at the depths of 0.40 to 1.25 m. The lower complex geochemical (alkaline and sorption) and mechanical barriers are located at the bottom part of the peat deposit (the depth of 2.25-2.50 m).

Язык оригинала	Английский
Номер статьи	01045
Журнал	E3S Web of Conferences
Том	98
DOI	https://doi.org/10.1051/e3sconf/20199801045
Состояние	Опубликовано - 7 июн 2019
Событие	16th International Symposium on Water-Rock Interaction, WRI 2019 and 13th International Symposium on Applied Isotope Geochemistry, 1st IAGC International Conference - Tomsk, Российская Федерация Продолжительность: 21 июл 2019 → 26 июл 2019

ASJC Scopus subject areas

Environmental Science(all)
Energy(all)
Earth and Planetary Sciences(all)

Доступ к документу

10.1051/e3sconf/20199801045

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title = "Water-rock interaction within the oligotrophic peat bog (part of the Vasyugan Swamp, Western Siberia)",

abstract = "Geochemical conditions of the formation of various minerals were studied within the oligotrophic pine-shrub and sphagnum peat bog. It was shown that at least two complex barriers function within the peat deposit. These barriers correspond to the changes in the advective and diffusion transfer of substances and promote the immobilization of Fe and a number of other chemical elements. The upper complex geochemical (redox, sulfide and sorption) barrier occurs approximately at the depths of 0.40 to 1.25 m. The lower complex geochemical (alkaline and sorption) and mechanical barriers are located at the bottom part of the peat deposit (the depth of 2.25-2.50 m).",

author = "Oleg Savichev and Aleksey Mazurov and Maxim Rudmin and Evgeniya Soldatova",

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T1 - Water-rock interaction within the oligotrophic peat bog (part of the Vasyugan Swamp, Western Siberia)

AU - Savichev, Oleg

AU - Mazurov, Aleksey

AU - Rudmin, Maxim

AU - Soldatova, Evgeniya

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N2 - Geochemical conditions of the formation of various minerals were studied within the oligotrophic pine-shrub and sphagnum peat bog. It was shown that at least two complex barriers function within the peat deposit. These barriers correspond to the changes in the advective and diffusion transfer of substances and promote the immobilization of Fe and a number of other chemical elements. The upper complex geochemical (redox, sulfide and sorption) barrier occurs approximately at the depths of 0.40 to 1.25 m. The lower complex geochemical (alkaline and sorption) and mechanical barriers are located at the bottom part of the peat deposit (the depth of 2.25-2.50 m).

AB - Geochemical conditions of the formation of various minerals were studied within the oligotrophic pine-shrub and sphagnum peat bog. It was shown that at least two complex barriers function within the peat deposit. These barriers correspond to the changes in the advective and diffusion transfer of substances and promote the immobilization of Fe and a number of other chemical elements. The upper complex geochemical (redox, sulfide and sorption) barrier occurs approximately at the depths of 0.40 to 1.25 m. The lower complex geochemical (alkaline and sorption) and mechanical barriers are located at the bottom part of the peat deposit (the depth of 2.25-2.50 m).

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