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

被引：2

作者：

Savichev, Oleg ^{[1
]}

Mazurov, Aleksey ^{[1
]}

Rudmin, Maxim ^{[1
]}

Soldatova, Evgeniya ^{[1
]}

机构：

[1] Tomsk Polytech Univ, Sch Earth Sci & Engn, Dept Geol, Lenina Ave 30, Tomsk 634050, Russia

来源：

16TH INTERNATIONAL SYMPOSIUM ON WATER-ROCK INTERACTION (WRI-16) AND 13TH INTERNATIONAL SYMPOSIUM ON APPLIED ISOTOPE GEOCHEMISTRY (1ST IAGC INTERNATIONAL CONFERENCE) | 2019年 / 98卷

基金：

俄罗斯基础研究基金会; 俄罗斯科学基金会;

关键词：

CHEMICAL-COMPOSITION; DEPTH;

D O I：

10.1051/e3sconf/20199801045

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

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).

引用

页数：6

共 29 条

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