Characterization of dissolved organic carbon (DOC) in a dystrophic lake and an adjacent fen

被引:0
作者
A. Sachse
D. Babenzien
G. Ginzel
J. Gelbrecht
C.E.W. Steinberg
机构
[1] Institute of Freshwater Ecology and Inland Fisheries (IGB),Chemical Laboratory
[2] Institute of Freshwater Ecology and Inland Fisheries (IGB),Department of Limnology of Stratified Lakes
[3] Institute of Freshwater Ecology and Inland Fisheries (IGB),Department of Ecohydrology
[4] Institute of Freshwater Ecology and Inland Fisheries (IGB),Chemical Laboratory
[5] Institute of Freshwater Ecology and Inland Fisheries (IGB),undefined
来源
Biogeochemistry | 2001年 / 54卷
关键词
catchment effects; DOC; humic substances; microbial degradation; oligotrophic acidic fen; polysaccharides;
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中图分类号
学科分类号
摘要
Dissolved organic carbon (DOC), humicsubstances (HS), polysaccharides (PS) and lowmolecular weight acids (LMWA) werecharacterized in water from the dystrophicLake Große Fuchskuhle over a period ofseven months. In addition, porewater from anadjacent fen was investigated in order toobtain information about the DOC in thecatchment area. Size-exclusion-chromatographycombined with UV- and organic carbon(IR)-detection was used to quantify DOC andits fractions. The lake had previously beendivided into four separate sections by largesheets of plastic, and the DOC compositiondiffered markedly between the fourcompartments. Spatial variations in HS and PSconcentrations were greater than seasonalvariations. The high amounts of HS (up to58%) in the western sections of the lake,indicated influence by subsurface water fromthe fen, whereas the eastern sections weredominated by PS (up to 35%) of algal origin.These differences could be explained byhydrological conditions, indicating thatcompletely different catchment areasinfluenced the water chemistry in the separatecompartments. By characterizing the HS bytheir average molecular weight and theiraromaticity, three different groups of HScould be distinguished depending on theirorigin and fate. Microbial degradation of DOCand its fractions differed between two of thecompartments during incubation studies over aperiod of six weeks.
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页码:279 / 296
页数:17
相关论文
共 61 条
[1]  
Amon RMW(1996)Bacterial utilization of different size classes of dissolved organic matter Limnol. Oceanogr. 41 41-51
[2]  
Benner R(1990)Microbial activities in a naturally acidotrophic lake Arch. Hydrobiol. Beih. Ergebn. Limnol. 34 175-181
[3]  
Babenzien HD(2000)Photochemical transformation of dissolved organic matter in lakes Limnol. Oceanogr. 45 753-762
[4]  
Babenzien C(1991)Evaluation ans application of dialysis porewater samplers for microbiological studies of sediment-water interfaces Aquatic Science 53/1 55-73
[5]  
Bertilsson S(1984)Interstitial water sampling by dialysis: Methodically notes Limnol. Oceanogr. 29 667-670
[6]  
Tranvik L. J.(1996)Seasonal variation in the composition of aquatic organic matter in some Nova Scottish brownwaters: a nuclear magnetic resonance approach Hydrobiol. 317 141-150
[7]  
Brandl H(1984)Sources and molecular weight of ‘dissolved’ organic carbon in an oligotrophic lake OIKOS 42 1-9
[8]  
Hanselmann KW(1994)Diagenesis of organic matter in a wetland receiving hypereutrophic lake water: II Role of inorganic electron acceptors in nutrient release J. Environ. Qual. 23 937-943
[9]  
Carignan R(1992)Impacts of environmental changes on the biogoechemistry of aquatic humic substances Hydrobiol. 229 59-71
[10]  
Clair TA(1976)An in situ sampler for close interval porewater studies Limnol. Oceanogr. 21 912-914