Abstract
Dissolved organic matter was studied in soils of the felled areas in fir-spruce forests of the southern Sikhote-Alin Ridge. After cutting of the forest, the molecular-mass characteristics of the dissolved organic matter in the soils changed: its molecular structure became simpler, and the degree of aromatic polycondensation and the capacity for the formation of complexes with Fe and Al decreased.
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Original Russian Text © T.N. Lutsenko, V.S. Arzhanova, N.Yu. Kim, 2006, published in Pochvovedenie, 2006, No. 6, pp. 674–680.
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Lutsenko, T.N., Arzhanova, V.S. & Kim, N.Y. Transformation of dissolved organic matter in soils of the felled areas in fir-spruce forests (Primorskii Krai). Eurasian Soil Sc. 39, 604–610 (2006). https://doi.org/10.1134/S1064229306060044
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DOI: https://doi.org/10.1134/S1064229306060044