Abstract
Behavior of iron forms and its differentiation in the soil profile in embryozems of different soil-climatic zones of the Kuznetsk Basin are considered for the first time as a diagnostic indicator of the character, intensity, and direction of soil processes.
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References
A. P. Zakharov, in Revegetation of the Disturbed Lands in Siberia (Kemerovo, 2006), Vol. 2, pp. 22–28 [in Russian].
A. V. Sokolov, in Proceedings of the 10th International Congress of Soil Science (Moscow, 1974), p. 4 [in Russian].
G. I. Makhonina, in Development of Disturbed Lands (Moscow, 1976), pp. 44–55 [in Russian].
A. A. Rode, Soil-Formation and Evolution of Soil (Moscow, 1947) [in Russian].
V. M. Kurachev and V. A. Androkhanov, Sibirskii Ekologicheskii Zh. 9(3), 255 (2002).
V. A. Androkhanov, E. D. Kulyapina, and V. M. Kurachev, Soils of Anthropogenic Landscapes: Genesis and Evolution (Novosibirsk, 2004) [in Russian].
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Original Russian Text © V.G. Dvurechenskii, 2009, published in Sibirskii Ekologicheskii Zhurnal, 2009, Vol. 16, No. 2, pp. 171–177.
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Dvurechenskii, V.G. Group composition of iron and humus in the soils of anthropogenic landscapes in the Kuznetsk Basin. Contemp. Probl. Ecol. 2, 645–649 (2009). https://doi.org/10.1134/S1995425509060241
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DOI: https://doi.org/10.1134/S1995425509060241