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Biogeosciences Discuss., 5, 2049-2073, 2008
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The relevance of particulate organic carbon (POC) for carbon composition in the pore water of drained and rewetted fens of the "Donauried" (South-Germany)

S. Fiedler1, B. S. Höll2, A. Freibauer3, K. Stahr1, M. Drösler4, M. Schloter5, and H. F. Jungkunst6
1Institute of Soil Science and Land Evaluation, Univ. of Hohenheim, Emil-Wolff-Strasse 27, 70599 Stuttgart, Germany
2Ludwig-Maximilians Univ., Dept. of Geography, Luisenstr. 37, 80333 Munich, Germany
3Max-Planck-Institute for Biogeochemistry, Postfach 100164, 07701 Jena, Germany
4Vegetation Ecology, Techn. Univ. of Munich, Am Hochanger 6, 85350 Freising, Germany
5Helmholtz Center Munich, German Research Center for Environmental Health (GmbH), Institute for Soil Ecology, Department for Terrestrial Ecotoxicology, Ingolstädter Landstr. 1, 85758 Oberschleissheim, Germany
6Landscape Ecology, Institute of Geography, University of G¨ ottingen, Goldschmidtstr. 5, 37077 Göttingen, Germany

Abstract. Numerous studies have dealt with carbon (C) concentrations in Histosols, but there are no studies quantifying the relative importance of all individual C components in pore waters. For this study, measurements were made of all the carbon components (i.e., particulate organic carbon, POC; dissolved organic carbon, DOC; dissolved inorganic carbon, DIC; dissolved methane, CH4) in the soil pore water of a calcareous fen under three different water management regimes (re-wetted, deeply and moderately drained). Pore water was collected weekly or biweekly (April 2004 to April 2006) at depths between 10 and 150 cm.

The main results obtained were: (1) DIC (94–280 mg C l−1) was the main C-component. (2) POC and DOC concentrations in the pore water (14–125 mg C l−1 vs. 41–95 mg C l−1) were pari passu. (3) Dissolved CH4 was the smallest C component (0.005–0.9 mg C l−1). Interestingly, about 30% of the POM particles were colonized by microbes indicating that they are active in the internal C transfer in the soil profile ("C-Shuttles"). Consequently, it was concluded that POC is at least as important as DOC for internal soil C turnover. There is no reason to assume significant biochemical differences between POC and DOC as they only differ in size. Therefore, both POC and DOC fractions are essential components of C budgets of peatlands. Furthermore dissolved CO2 in all forms of DIC apparently is an important part of peatland C-balances.


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Citation: Fiedler, S., Höll, B. S., Freibauer, A., Stahr, K., Drösler, M., Schloter, M., and Jungkunst, H. F.: The relevance of particulate organic carbon (POC) for carbon composition in the pore water of drained and rewetted fens of the "Donauried" (South-Germany), Biogeosciences Discuss., 5, 2049-2073, 2008.   Bibtex   EndNote   Reference Manager