GEOCHEMICAL PECULIARITIES OF TOP PEAT IN MIDDLE TAIGA OF THE PRE-OB REGION

The top peat in middle taiga of the Pre-Ob region represents a highly negative geochemical anomaly of several chemical elements as compared to that in southern taiga located in the middle and upper parts of this region. Obviously, due to close location of mountain systems (Altai, Salair ridge, Kuzne...

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Bibliographic Details
Published in:Dokuchaev Soil Bulletin
Main Authors: Yu. N. Vodyanitsky, A. T. Savichev, N. F. Avetov, S. Ya. Trofimov, S. A. Kozlov
Format: Article in Journal/Newspaper
Language:Russian
Published: V.V. Dokuchaev Soil Science Institute 2012
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Online Access:https://doi.org/10.19047/0136-1694-2012-69-34-45
https://doaj.org/article/4520a630604440f8b1f73233841c8d99
Description
Summary:The top peat in middle taiga of the Pre-Ob region represents a highly negative geochemical anomaly of several chemical elements as compared to that in southern taiga located in the middle and upper parts of this region. Obviously, due to close location of mountain systems (Altai, Salair ridge, Kuznetsk Alatau) and the aerial dust transfer the top peat in southern taiga is enriched with the major metals; this process is unachievable for the remote middle part of the Pre-Ob region.