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Strong negative geochemical anomaly of raised bog peat in the middle taiga zone, Middle Priobye

  • Genesis and Geography of Soils
  • Published:
Moscow University Soil Science Bulletin Aims and scope

Abstract

Peat samples from bogs of the middle taiga zone (Middle Priobye region) represent a strong negative geochemical anomaly of a number of chemical elements compared to peat samples from bogs of the southern taiga of the Middle and Upper Priobye regions.

The proximity of mountain systems (the Altai Mountains, the Salair Ridge, and Kuznetskii Alatau) presumably affects peat composition in the southern taiga zone by air transportation of mineral dust. The latter fact enriches peat of raised bogs in certain metals, whilst not reaching the outlying Middle Priobye region.

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Authors and Affiliations

  1. Dokuchaev Soil Science Institute, Russian Academy of Agricultural Sciences, Moscow, Russia

    Yu. N. Vodyanitskii

  2. Geological Institute, Russian Academy of Sciences, Moscow, Russia

    A. T. Savichev

  3. Faculty of Soil Science, Moscow State University, Moscow, Russia

    N. A. Avetov, S. Ya. Trofimov & S. A. Kozlov

Authors
  1. Yu. N. Vodyanitskii
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  2. A. T. Savichev
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  3. N. A. Avetov
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  4. S. Ya. Trofimov
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  5. S. A. Kozlov
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Correspondence to Yu. N. Vodyanitskii.

Additional information

Original Russian Text © Yu.N. Vodyanitskii, A.T. Savichev, N.A. Avetov, S.Ya. Trofimov, S.A. Kozlov, 2012, published in Vestnik Moskovskogo Universiteta. Pochvovedenie, 2012, No. 3, pp. 3–8.

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Vodyanitskii, Y.N., Savichev, A.T., Avetov, N.A. et al. Strong negative geochemical anomaly of raised bog peat in the middle taiga zone, Middle Priobye. Moscow Univ. Soil Sci. Bull. 67, 111–116 (2012). https://doi.org/10.3103/S0147687412030076

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  • DOI: https://doi.org/10.3103/S0147687412030076

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