Journal of Forest Research · 2011 · 22 citations · 44 references
AgricultureEarth SciencesSoil SciencesSoil ChemistrySoil Organic MatterSoil SciencePlant-soil InteractionsSoil Chemical PropertiesSoil Organic Matter ChemistrySoil Organic Matter FractionsHumus CharacterizationNuclear Magnetic Resonance SpectroscopyOrganic ContentOrganic Matter HumificationSoil Organic CarbonSoil Organic Carbon FractionsSoil Organic Matter CharacterizationSoil Organic Matter Spectroscopy
AbstractWe investigated soil organic matter in a forest of natural Hinoki cypress (Chamaecyparis obtusa) under perhumid weather conditions in north central Taiwan. Humic substances along the transect from the summit and footslope to lakeshore were characterized by use of solid-state cross-polarization, magic-angle-spinning 13C nuclear magnetic resonance spectroscopy (CP/MAS 13C-NMR). The major components of soil organic carbon in whole soil and humic substances were alkyl-C, O-alkyl-C, and di-O-alkyl-C, ranging from 60.6% to 80.7%, then aromatic-C, 7.5% to 9.8%. The degree of humification of soil organic matter, both O-alkyl-C/alkyl-C ratio and aromaticity, decreased slightly from the summit to lakeshore. The content of functional groups of polar and acidic groups, including O-alkyl-C, di-O-alkyl-C, and carboxyl-C, corresponded with the topographical effect, increasing slightly from the summit to lakeshore. However, the relatively low degree of humification in soils of this perhumid forest and low aromaticity were due to high precipitation and acidity, which appeared to hinder organic matter decomposition with topography change.Keywords: CP/MAS 13C-NMRForest soilsFulvic acidsHumic acids
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