Abstract
A total of 123 humic acid isolates from terrestrial and marine, mostly North Sea, sources was analysed by Fourier-transform infrared (FT-IR) spectroscopy. The spectra were found to be strongly influenced by co-extracted clay minerals. After treatment with hydrofluoric acid the ash content of the isolates was reduced considerably. Interferences from inorganic compounds were also eliminated. IR spectra of humic acids of marine and terrestrial origin show characteristic differences only in the region below 2000 cm−1. Although marine humic acids tend to contain more protein-related functions, it is not possible to distinguish marine and terrestrial samples by FT-IR spectroscopy alone. A combination with other suitable parameters, e.g. IR and UV/Vis absorbance data (A270 nm/A407 nm), helps to specify different sources of humic materials.
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References
Baruah, M. K. (1986): Assignment of the IR absorption band at 1050 cm−1 in lignite humic acid. — Fuel,65: 1756–1759.
Bellamy, L.J. (1975): The Infrared Spectra of Complex Molecules. 3rd ed. — 433 pp; London (Chapman & Hall).
Belzile, N. &Joly, H. A. &Li, H. (1997): Characterization of humic substances extracted from Canadian lake sediments. — Can. J. Chem.,75: 14–27.
Dereppe, J.-M. &Moreaux, C. &Debyser, Y. (1980): Investigation of marine and terrestrial humic substances by1H and13C nuclear magnetic resonance and infrared spectroscopy. — Org. Geochem.,2: 117–124.
Durand, B. &Nicaise, G. (1980): Procedures for kerogen isolation. — In:Durand, B. [Ed.]: Kerogen — Insoluble Organic Matter from Sedimentary Rocks: 35–53; Paris (Edn. Technip).
Ertel, J. R. &Hedges, J. I. (1983): Bulk chemical and spectroscopic properties of marine and terrestrial humic acids, melanoidins and catechol-based synthetic polymers. — In:Christman, R. F. &Gjessing, E. T. [Eds.]: Aquatic and Terrestrial Humic Materials: 143–163; Michigan (Ann Arbor Sci.).
Filip, Z. &Alberts, J.J. (1994): Adsorption and transformation of salt marsh related humic acids by quartz and clay minerals. — Sci. Total Environ.,153: 141–150.
Fooken, U. &Liebezeit, G. (2000): Distinction of marine and terrestrial origin of humic acids in North Sea surface sediments by absorption spectroscopy. — Mar. Geol.,164: 173–181.
Fooken, U. (1999): Huminsäuren in Oberflächensedimenten der Nordsee — Indikatoren für terrestrischen Eintrag? — Dissertation Thesis Carl von Ossietzky-Univ. Oldenburg: 159 pp.
Francioso, O. &Ciavatta, C. &Tugnoli, V. &Sánchez-Cortés, S. &Gessa, C. (1998a): Spectroscopic characterization of pyrophosphate incorporation during extraction of peat humic acids. — Soil Sci. Amer. J.,62: 181–187.
Francioso, O. &Sanchez-Cortés, S. &Tugnoli, V. &Ciavatta, C. &Gessa, C. (1998b): Characterization of peat fulvic acid fractions by means of FT-IR, SERS and1H,13C NMR spectroscopy. — Appi. Spectr.,52: 270–277.
Gerasimowicz, W. V. &Byler, D. M. (1985):13C CPMAS NMR and FT-IR spectroscopic studies of humic acids. — Soil Sci.,139: 270–278.
Hedges, J. I. &Keil, R. G. &Benner, R. (1997): What happens to terrestrial organic matter in the ocean? — Org. Geochem.,27: 195–212.
Huc, A. Y. &Durand, B. M. (1977): Occurrence and significance of humic acids in ancient sediments. — Fuel,56: 73–80.
Ishiwatari, R. (1970): Structural characteristics of humic substances in recent lake sediments. — In:Hobson, G. D. &Speers, G. C. [Eds.]: Advances in Organic Geochemistry: 283–311. Oxford (Pergamon).
Lynch, B. M. &Smith-Palmer, T. (1992): Interpretation of FTIR spectral features in the 1000–1200 cm−1 region in humic acids: contributions from particulate silica in different sampling media. — Can. J. Appi. Spec,37: 126–131.
MacCarthy, P. &Rice, J. A. (1985): Spectroscopic methods (other than NMR) for determining functionality in humic substances. — In:Aiken, G. R. &McKnight, D. M. &Wershaw, R. L. &MacCarthy, P. [Eds.]: Humic Substances in Soil, Sediment and Water: 527–559; New York (Wiley & Sons).
Marel, H. W. van der &Beutelspacher, H. (1976): Atlas of Infrared Spectroscopy of Clay Minerals and their Admixtures. — 396 pp; Amsterdam (Elsevier).
Niemeyer, J. &Chen, Y. &Bollag, J.-M. (1992): Characterization of humic acids, composts, and peat by diffuse reflectance Fourier-transform infrared spectroscopy. — Soil Sci. Am. J.,56: 135–140.
Piccolo, A. &Rausa, R. &Calemma, V. (1989): FT-IR spectra of humic substances extracted with dipolar aprotic solvents. — Chemosphere,18: 1927–1933.
Senesi, N. &Miano, T. M. &Provenzano, M. R. &Brunetti, G. (1989): Spectroscopic and compositional comparative characterization of I.H.S.S. reference and standard fulvic and humic acids of various origin. — Sci. Total Environ.,81/82: 143–156.
Stevenson, F.J. &Goh, K. M. (1971): Infrared spectra of humic acids and related substances. — Geochim. Cosmochim. Acta,35: 471–483.
Stevenson, F.J. (1982): Humus Chemistry Genesis, Composition, Reactions. — 443 pp; New York (Wiley & Sons).
Volkman, J. K. &Rohjans, D. &Rullkötter, J. &Scholz-Böttcher, B. M. &Liebezeit, G. (2000): Sources and diagenesis of organic matter in tidal flat sediments from the German Wadden Sea. — Cont. Shelf Res.,20: 1139–1158.
Yonebayashi, K. &Hattori, T. (1989): Chemical and biological studies on environmental humic acids. — Soil Sci. Plant Nutr.,35: 383–392.
Yunoian, T. &Ming, G. &Bing, L. (1986): Humic substances in sediments. — Acta Oceanol. Sin.,5: 235–246.
Zöllmer, V. &Irion, G. (1993): Clay mineral and heavy metal distributions in the northeastern North Sea. — Mar. Geol.,111: 223–230.
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Fooken, U., Liebezeit, G. An IR study of humic acids isolated from sediments and soils. Senckenbergiana maritima 32, 183–189 (2003). https://doi.org/10.1007/BF03043094
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DOI: https://doi.org/10.1007/BF03043094