4.7 Article

Characterization and acid-base properties of fulvic and humic acids isolated from two horizons of an ombrotrophic peat bog

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GEODERMA
卷 126, 期 3-4, 页码 367-374

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ELSEVIER SCIENCE BV
DOI: 10.1016/j.geoderma.2004.10.006

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peat fulvic acid; peat humic acid; elemental and ftinctional composition; FTIR spectroscopy; NMR spectroscopy; acid properties; soil depth effect

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Peat humic and fulvic acids were isolated from a surface horizon (0-60 cm) and deeper horizon (> 60 cm) of an ombrotrophic peat bog located in Galicia (NW Spain) and which constitutes a record of pateoenvironmental contamination. The humic and fulvic acids were characterized and compared using chemical methods and spectroscopic techniques, including ultraviolet visible (UV-vis), Fourier transform infrared (FTIR) and C-13 nuclear magnetic resonance (C-13 NMR). Comparison of the E-4/E-6 ratios showed that in the deeper horizon the peat humic substances have a greater degree of aromatic condensation than in the surface horizon. The alkyl C content of the humic substances remained practically unchanged, whereas the O-alkyl-C content of humic acids decreased with depth. No variation with depth in the ionization constants of the carboxylic groups or of the phenolic groups was observed. The values of the ratios of the carboxylic/phenolic contents were similar to those reported in the available literature, with a higher content of acid groups in the humic substances isolated from the lower horizon mainly attributable to the carboxylic groups. (c) 2004 Elsevier B.V. All rights reserved.

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