Hydromorphism and Al-Fe-humus pedogenesis on sandy parent materials in the Kola Peninsula |
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| Authors: | V. N. Perverzev T. I. Litvinova |
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| Affiliation: | (1) Avrorin Polar-Alpine Botanical Garden, Kola Research Center of the Russian Academy of Sciences, Kirovsk, Murmansk oblast, 184230, Russia |
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| 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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