Potential rates of nitrification and denitrification in an oligotrophic freshwater sediment system |
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Authors: | Walter K. Dodds Ronald D. Jones |
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Affiliation: | (1) Department of Biology, University of Oregon, 97403 Eugene, Oregon;(2) Department of Microbiology, Oregon State University, 97331 Corvallis, Oregon, USA;(3) Present address: Department of Biological Sciences, Florida International University, 33199 Miami, Florida, USA |
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Abstract: | Potential rates of nitrification and denitrification were measured in an oligotrophic sediment system. Nitrification potential was estimated using the CO oxidation technique, and potential denitrification was measured by the acetylene blockage technique. The sediments demonstrated both nitrifying and denitrifying activity. Eh, O2, and organic C profiles showed two distinct types of sediment. One type was low in organic C, had high O2 and Eh, and had rates of denitrification 1,000 times lower than the other which had high organic C, low O2, and low Eh. Potential nitrification and denitrification rates were negatively correlated with Eh. This suggests that environmental heterogeneity in denitrifier and nitrifier populations in oligotrophic sediment systems may be assessed using Eh before sampling protocols for nitrification or denitrification rates are established. There was no correlation between denitrification and nitrification rates or between either of these processes and NH4+ or NO3– concentrations. The maximum rate of denitrification was 0.969 nmole N cm–3 hour–1, and the maximum rate of nitrification was 23.6 nmole cm–3 hour–1, suggesting nitrification does not limit denitrification in these oligotrophic sediments. Some sediment cores had mean concentrations of 6.0 mg O2/liter and still showed both nitrification and denitrification activity. |
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