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Spectroscopic properties of dissolved humic substances - a reflection of land use history in a fen area

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Abstract

The elemental composition and spectroscopic properties of dissolved fulvic acids isolated from different sampling media (topsoil, ground and surface water) of a natural fen area (high portion of organic soils) were examined to reveal the effects of land use history. These effects need to be known if dissolved humic substances are to be a major factor in identifying the impact of present and future changes in land use. Dissolved fulvic acids (topsoil, groundwater) from highly degraded peatlands (due to a long-term agricultural use) exhibit lower C/N ratios, higher absorption in the UV spectra, and higher absorption at 1,620 cm−1 in the FTIR spectra compared with fulvic acids from relatively intact peatlands. These properties illustrate that long-term agricultural use with high inputs results in increased aromatic structures and a further humification of dissolved fulvic acids due to very strong peat decomposition compared with relatively intact peatlands. Synchronous fluorescence spectra also indicate the higher level of aromatic structures within fulvic acids isolated from sites with long-term agricultural use (high peat decomposition) compared with a land use history resulting in a lower peat decomposition. The different sources of fulvic acids in surface water (precipitation, runoff, interflow, groundwater) are the main reason for these effects not being detected in fulvic acids isolated from surface water. Short-term changes in land use characterized by a transition from crop farming to an unimproved grassland were found not to affect the spectroscopic properties of dissolved fulvic acids. A humification index deduced from the synchronous fluorescence spectra is proposed. We have strong evidence that dissolved humic substances indicate changes in the environmental conditions (both anthropogenic and natural) of wetlands with a high proportion of organic soils.

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References

  • Aiken G, McKnight D, Harnish R & Wershaw R (1996) Geochemistry of aquatic humic substances in the Lake Fryxell Basin, Antarctica. Biogeochemistry 34: 157-188

    Google Scholar 

  • Altermann M & Refior K (1997) Die Moorböden des Drömlings — gegenwärtiger Zustand — Prognose — Bodenschutz. Mittlgn. Deutsch. Bodenk. Gesell. 85: 1091-1094

    Google Scholar 

  • Anonymus (1996) Pflege-und Entwicklungsplan für das Naturschutzgroßprojekt Drömling, Teilvorhaben Sachsen-Anhalt, Kurzfassung (pp 1-88). Ministerium für Raumordnung, Landwirtschaft und Umwelt Sachsen-Anhalt

  • Buffle J, Deladoey P, Zumstein J & Haerdi W (1982) Analysis and characterization of natural organic matters in freshwaters. I. Study of analytical techniques. Schweiz. Z. Hydrol. 44(2): 325-362

    Google Scholar 

  • Capriel, P (1997) Hydrophobicity of organic matter in arable soils: influence of management. Eur. J. Soil. Sci. 48: 457-462

    Google Scholar 

  • Chin Y-P, Aiken G & Loughlin EO (1994) Molecular weight, polydispersity, and spectroscopic properties of aquatic humic substances. Environ. Sci. Technol. 28: 1853-1858

    Google Scholar 

  • Chittleborough DJ, Smettem KRJ, Cotsaris E & Leaney FW (1992) Seasonal changes in pathways of dissolved organic carbon through a hillslope soil (xeralf) with contrasting texture. Aust. J. Soil Res. 30: 465-476

    Google Scholar 

  • Cronan CS, Lakshman S & Patterson HH (1992) Effects of disturbance and soil amendments on dissolved organic carbon and organic acidity in red pine forest floors. J. Environ. Qual. 21: 457-463

    Google Scholar 

  • Dalva M & Moore TR (1991) Sources and sinks of dissolved organic carbon in a forested swamp catchment. Biogeochem. 15: 1-19

    Google Scholar 

  • Erich MS & Trusty GM (1997) Chemical characterization of dissolved organic matter released by limed and unlimed forest soil horizons. Can. J. Soil. Sci. 77(3): 405-413

    Google Scholar 

  • FAO (1990) Soil Map of the World. Revised Legend. World Soil Resources Report 60, Rom

  • Gehring AU, Guggenberger G, Zech W & Luster J (1997) Combined magnetic, spectroscopic, and analytical-chemical approach to infer genetic information for a vertisol. Soil. Sci. Soc. Am. J. 61: 78-85

    Google Scholar 

  • Geyer S, Kalbitz K & Geyer W (1998) The influence of changing land use in a fen area on the isotopic (14C) and chemical signature of DOC — Conclusions for the initial 14C content of DOC for groundwater dating. Isotope Techniques in the Study of Environmental Change (Proc. Symp. Vienna, 1997) (pp 780-785). IAEA, Vienna

    Google Scholar 

  • Geyer W, Brüggemann L & Hanschmann G (1998) Prediction of properties of soil humic substances from FTIR spectra using partial least squares regression. International J. Environ. Anal. Chem. 71(2): 181-193

    Google Scholar 

  • Gu B, Schmitt J, Chen Z, Liang L & McCarthy JF (1995) Adsorption and desorption of different organic matter fractions on iron oxide. Geochim. Cosmochim. Acta 59: 219-229

    Google Scholar 

  • Guggenberger G, Christensen BT & Zech W (1994) Land-use effects on the composition of organic matter in particle size separates of Soil: I. Lignin and carbohydrate signature. European Journal of Soil Science 45: 449-458

    Google Scholar 

  • Homann PS & Grigal DF (1992) Molecular weight distribution of soluble organics from laboratory-manipulated soils. Soil Sci. Soc. Am. J. 56: 1305-1310

    Google Scholar 

  • Hunchak-Kariouk K & Suffet, IH (1994) Binding of organic pollutants to dissolved organic matter in anoxic pore waters. In: Senesi N & Miano TM (Eds) Humic Substances in the Global Environment and Implications on Human Health (pp 1031-1036). Elsevier, Amsterdam

    Google Scholar 

  • Jardine PM, Weber NL & McCarthy JF (1989) Mechanism of dissolved organic carbon adsorption on soil. Soil Sci. Soc. Am. J. 53: 1378-1385

    Google Scholar 

  • Kaiser K & Zech W (1997) Natural organic matter sorption on different mineral surfaces studied by DRIFT spectroscopy. Sciences of Soils 2: http://www.hintze-online.com/sols/1997/Article s/Art4

  • Kalbitz K & Wennrich R (1998) Mobilization of heavy metals and arsenic in polluted wetland soils and its dependence on dissolved organic matter. Sci. Total Environ. 209(1): 27-39

    Google Scholar 

  • Kalbitz K, Geyer S, Geyer W, Rupp H, Knappe S, Meißner R & Braumann F (1997) Land use effects on dissolved organic matter in the unsaturated and saturated zone of a fen area. In: Frimmel F & Abbt-Braun G (Eds) Symposium on Refractory Organic Substances in the Environment — ROSE (pp 156-158). Wasserchemie Karlsruhe, Heft 35, Engler-Bunte-Inst., Univ. Karlsruhe

  • Kögel-Knabner I, Zech W & Hatcher PG (1988) Chemical composition of the organic matter in forest soils. III. The humus layer. Z. Pflanzenernaehr. Bodenk. 151: 331-340

    Google Scholar 

  • Koerschens M, Weigel, A & Schulz E (1998) Turnover of soil organic matter (SOM) and longterm balances — tools for evaluating sustainable productivity of soils. Z. Pflanzenernaehr. Bodenk. 161: 409-424

    Google Scholar 

  • Kreutzer K (1995) Effects of liming on soil processes. Plant and Soil 168–169: 447-470

    Google Scholar 

  • Leenheer JA (1981) Comprehensive approach to preparative isolation and fractionation of dissolved organic carbon from natural waters and wastewaters. Environ. Sci. Technol. 15: 578-587

    Google Scholar 

  • Li Z & Shuman LM (1997) Mobility of Zn, Cd, and Pb in soils as affected by poultry litter extract, I. leaching in soil columns. Environ. Pollut. 95: 219-226

    Google Scholar 

  • Liechty HO, Kuuseoks E & Mroz GD (1995) Dissolved organic carbon in northern hardwood stands with differing acidic inputs and temperature regimes. J. Environ. Qual. 24: 927-933

    Google Scholar 

  • McKnight DM, Bencala KE, Zellweger GW, Aiken GR, Feder GL & Thorn KA (1992) Sorption of dissolved organic carbon by hydrous aluminium and iron oxides occuring at the confluence of Deer Creek with the Snake river, Summit country, Colorado. Environ. Sci. Technol. 26: 1388-1396

    Google Scholar 

  • McKnight DM, Harnisch R, Wershaw RL, Baron JS & Schiff S (1997) Chemical characteristics of particulate, colloidal, and dissolved organic material in Loch Vale Watershed, Rocky Mountain National Park. Biogeochem. 36: 99-124

    Google Scholar 

  • Meissner R, Seeger J, Rupp H & Schonert P (1993) The influence of laying up and extensification on the nitrogen wash out with seepage water. Vom Wasser 81: 197-215

    Google Scholar 

  • Meissner R, Rupp H, Schonert P, Seeger J, Braumann F & Müller H (1995) Effects of extensification in the fen area “Droemling” on the nitrogen content of soil as well as ground and surface water. Arch. für Nat.-Lands. 33: 255-269

    Google Scholar 

  • Miano TM & Senesi N (1992) Synchronous excitation fluorescence spectroscopy applied to soil humic substances chemistry. Sci. Total Environ. 117(118): 41-51

    Google Scholar 

  • Mobed JJ, Hemmingsen SL, Autry JL & McGown LB (1996) Fluorescence characterization of IHSS humic substances: Total luminescence spectra with absorbance correction. Environ. Sci. Technol. 30: 3061-3065

    Google Scholar 

  • Mulholland PJ (1997) Dissolved organic matter concentration and flux in streams. J. North Am. Benthological Soc. 16: 131-141

    Google Scholar 

  • Parfitt RL, Theng BKG, Whitton JS & Shepherd TG (1997) Effects of clay minerals and land use on organic matter pools. Geoderma. 75: 1-12

    Google Scholar 

  • Peuravuori J & Pihlaja K (1997) Isolation and characterization of natural organic matter from lake water: comparision of isolation with solid adsorption and tangential membrane filtration. Environ. Int. 23: 441-451

    Google Scholar 

  • Senesi N (1990) Molecular and quantitative aspects of the chemistry of fulvic acid and its interactions with metal ions and organic chemicals. Part II. The fluorescence spectroscopy approach. Analytica Chimica Acta 232: 77-106

    Google Scholar 

  • Senesi N, Miano TM & Brunetti G (1996) Humic-like substances in organic amendments and effects on native soil humic substances. In: Piccolo A (Ed) Humic Substances in Terrestrial Ecosystems (pp 531-593). Elsevier, Amsterdam

    Google Scholar 

  • Senesi N, Miano TM, Provenzano MR & Brunetti G (1991) Characterization, differentiation, and classification of humic substances by fluorescence spectroscopy. Soil Sci. 152: 259-271

    Google Scholar 

  • Senesi N, Miano TM, Provenzano MR & 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

    Google Scholar 

  • Stevenson FJ & Goh KM (1971) Infrared spectra of humic acids and related substances. Geochim. Cosmochim. Acta 35: 471-483

    Google Scholar 

  • Tegen I & Dörr H (1996) Mobilization of cesium in organic rich soils: correlation with production of dissolved organic carbon. Water Air Soil Pollut. 88: 133-144

    Google Scholar 

  • Thurman EM & Malcolm RL (1981) Preparative isolation of aquatic humic substanes. Environ. Sci. Technol. 15: 463-466.

    Google Scholar 

  • Thurman EM, Wershaw RL, Malcolm RL & Pinckney DJ (1982) Mocecular size of aquatic humic substances. Org. Geochem. 4: 27-35

    Google Scholar 

  • Wassenaar LI (1990) Geochemistry, Isotopic Composition, Origin, and Role of Dissolved Organic Carbon Fractions in Groundwater Systems. PhD thesis, University of Waterloo, Ontario, Canada

    Google Scholar 

  • Zech W, Senesi N, Guggenberger G, Kaiser K, Lehmann J, Miano TM, Miltner A & Schroth G (1997) Factors controlling humification and mineralization of soil organic matter in the tropics. Geoderma 79: 117-161

    Google Scholar 

  • Zsolnay A (1996) Dissolved humus in soil waters. In: Piccolo A (Ed) Humic Substances in Terrestrial Ecosystems (pp 171-223). Elsevier, Amsterdam

    Google Scholar 

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Authors and Affiliations

  1. Bayreuth Institute of Terrestrial Ecosystem Research (BITDK), University of Bayreuth, Germany

    K. Kalbitz

  2. Department of Analytical Chemistry, UFZ Centre for Environmental Research, Permoserstr. 15, D-04318, Leipzig, Germany

    W. Geyer

  3. Department of Hydrogeology, UFZ Centre for Environmental Research, Theodor-Lieser-Strasse 4, D-06120, Halle (Saale), Germany

    S. Geyer

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  1. K. Kalbitz
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  2. W. Geyer
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  3. S. Geyer
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Correspondence to K. Kalbitz.

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Kalbitz, K., Geyer, W. & Geyer, S. Spectroscopic properties of dissolved humic substances - a reflection of land use history in a fen area. Biogeochemistry 47, 219–238 (1999). https://doi.org/10.1023/A:1006134214244

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