Abstract
It is shown that the lipid fraction of soil organic matter consists of molecular fragments of aliphatic, O,N-alkyl, aromatic, and carboxyl groups, chlorophyll and/or chlorophyll-like pigments. The 13C-NMR data show that an increase in the degree of hydromorphism leads to an increase in the proportion of unsaturated components (-C=C-; -Ar). The paramagnetic activity of lipids is assessed. It is established that unpaired electrons are present only in the structure of the lipid fraction of organogenic horizons.
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Original Russian Text © E.D. Lodygin, V.A. Beznosikov, 2010, published in Doklady Rossiiskoi Akademii Sel’skokhozyaistvennykh Nauk, 2010, No. 6, pp. 30–32.
This work was supported by the Russian Foundation for Basic Research (grant no. 07-04-00285.
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Lodygin, E.D., Beznosikov, V.A. Composition of soil organic matter lipids. Russ. Agricult. Sci. 36, 437–440 (2010). https://doi.org/10.3103/S1068367410060133
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DOI: https://doi.org/10.3103/S1068367410060133