Release:
2015, Vol. 1. №3(3)About the authors:
Dmitrii V. Moskovchenko, Dr. Sci. (Geogr.), Head of the Geoecology Sector, Tyumen Scientific Center of the Siberian Branch of the Russian Academy of Sciences; Lead Research Associate, Institute of Environmental and Agricultural Biology (X-BIO), University of Tyumen; moskovchenko1965@gmail.comAbstract:
The article presents the results of studies of the mobile forms of metals (Pb, Cu, Zn, Ni, Cr, Mn, Fe) in the soils of the taiga zone of Western Siberia. There is a significant variation in the elemental composition, the coefficients of variation greater than 100% due to the differences of the genesis of mineral and peat soils, the diversity of soil-forming rocks, the presence of geochemical barriers. For peat soils are essential processes of biological accumulation of elements, which leads to an increase in the concentration of zinc, lead and manganese. It is noted that the share of mobile forms of metals in soils of the Northern regions of Western Siberia more than in the southern forest-steppe and steppe, which is associated with the more acidic, the lack of carbonate rocks. Despite the lack of pollution sources, the observed number of cases exceeding MPC. Most often the excess observed for manganese (2.1% of analyzed samples). Cases of the maximum permissible concentration of elements such as Pb, Zn, Cu, Mn and Ni are more frequent in peat soils than in the mineral, which is due to bioaccumulation, sorption and accumulation of oxidative geochemical barrier.Keywords:
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