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Changes of humic substances characteristics from forested to cultivated soils in Ethiopia

The dynamics of the stable fractions of soil organic matter (SOM), the humic substances, has been rarely studied in tropical soils. We evaluated extraction yields, elemental composition, isotopic δ 13C abundance and solid-state 13C NMR spectra of humic fractions isolated from five forested and culti...

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Bibliographic Details
Published in:Geoderma 2006-05, Vol.132 (1), p.9-19
Main Authors: Spaccini, R., Mbagwu, J.S.C., Conte, P., Piccolo, A.
Format: Article
Language:English
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Summary:The dynamics of the stable fractions of soil organic matter (SOM), the humic substances, has been rarely studied in tropical soils. We evaluated extraction yields, elemental composition, isotopic δ 13C abundance and solid-state 13C NMR spectra of humic fractions isolated from five forested and cultivated soils in Ethiopia in order to assess the influence of deforestation and subsequent cultivation on the composition of humic fractions. In all locations, humic (HA) and fulvic (FA) acids, humin (HU) and a humic hydrophobic fraction extracted with an acetone–HCl solution (HE) were decreased as a result of deforestation and cultivation, but the magnitude of decrease was site-specific. While the elemental composition of HA, FA and HU did not vary significantly with land use, that of the hydrophobic HE generally decreased with deforestation. Cultivation varied the δ 13C values of humic fractions with location and their high values suggested a history of C4 plants incorporation in soil. The 13C NMR spectra of HA, FA and HU showed that hydrophobic components (HB) were generally lower than hydrophilic ones (HI), resulting in a degree of hydrophobicity (HB/HI) being
ISSN:0016-7061
1872-6259
DOI:10.1016/j.geoderma.2005.04.015