Soil Science · 1986 · 75 citations · 0 references
AgricultureEarth SciencesSoil SciencesSoil ChemistrySoil Organic MatterSoil ScienceHumus FormationOrganic Matter DecompositionSoil Carbon FractionationSoil Chemical PropertiesSoil Organic Matter ChemistrySoil Organic Matter FractionsHumus CharacterizationHumus CompositionIsoelectric FocusingOrganic ContentSoil Organic CarbonSoil Organic Matter CharacterizationSoil Organic Matter ContentUltrafiltration
We used the pyrolysis-gas chromatography technique (Py-GC) to characterize mature and immature soil organic matter (PN soil: C/N = 24.8; PS soil: C/N = 12.6). PN produced on pyrolysis an abundance of furfural and phenol, indicating the presence of partially decomposed litter. PS, on the contrary, produced a considerable amount of benzene, which was consistent with a more mature humus. The extracts were fractionated in HAs and FAs and by membrane ultrafiltration, in fractions A1 (mol wt > 105), A2 (>104), and R (<104). Extracts and relative fractions were characterized by Py-GC and isoelectric focusing (IEF). The elaboration of the relative abundances and several Py-GC ratios proved to be very appropriate in assessing differences or similarities among soils and their fractions. Independently of the maturity of soil humus, the A1s and HAs were carbohydrate-rich and composed of highly condensed humus; the Rs were polyphenol-rich, less condensed, and similar to FAs; the A2s showed intermediate properties. IEF has proved a reliable technique for characterizing structurally different organic fractions. The IEF patterns of the fractions were charge-size depenedent, and, on the basis of the charge and heterogeneity, they supported the Py-GC results.