Abstract
Al-Fe-humus podzols developed from sandy materials of continental and marine origins can be arranged into the following sequence with respect to the degree of soil hydromorphism: iron-illuvial podzols—humus-illuvial podzols—dark (high-humus) humus-illuvial podzols—peat podzols. These soils do not differ much in their particle-size distribution and bulk elemental composition. The most informative indices reflecting the effect of soil hydromorphism are the contents of oxalate-extractable iron and aluminum compounds and the contents and composition of the soil organic matter.
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Original Russian Text © V.N. Perverzev, T.I. Litvinova, 2008, published in Pochvovedenie, 2008, No. 7, pp. 773–782.
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Perverzev, V.N., Litvinova, T.I. Hydromorphism and Al-Fe-humus pedogenesis on sandy parent materials in the Kola Peninsula. Eurasian Soil Sc. 41, 677–685 (2008). https://doi.org/10.1134/S1064229308070016
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DOI: https://doi.org/10.1134/S1064229308070016