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

Research output: Contribution to journalConference article

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).

Original languageEnglish
Article number01045
JournalE3S Web of Conferences
Volume98
DOIs
Publication statusPublished - 7 Jun 2019
Event16th International Symposium on Water-Rock Interaction, WRI 2019 and 13th International Symposium on Applied Isotope Geochemistry, 1st IAGC International Conference - Tomsk, Russian Federation
Duration: 21 Jul 201926 Jul 2019

Fingerprint

Peat
water-rock interaction
peatland
swamp
peat
sorption
Rocks
Sorption
chemical element
Deposits
immobilization
Water
shrub
sulfide
Chemical elements
mineral
Minerals

ASJC Scopus subject areas

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

Cite this

Water-rock interaction within the oligotrophic peat bog (part of the Vasyugan Swamp, Western Siberia). / Savichev, Oleg; Mazurov, Aleksey; Rudmin, Maxim; Soldatova, Evgeniya.

In: E3S Web of Conferences, Vol. 98, 01045, 07.06.2019.

Research output: Contribution to journalConference article

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