Department of Biology, University of Oregon, 97403, Eugene, Oregon.
Microb Ecol. 1987 Jul;14(1):91-100. doi: 10.1007/BF02011574.
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.
在贫营养沉积物系统中测量了潜在的硝化和反硝化速率。硝化潜能使用 CO 氧化技术来估算,潜在的反硝化作用通过乙炔阻断技术来测量。沉积物表现出硝化和反硝化活性。Eh、O2 和有机 C 剖面显示了两种不同类型的沉积物。一种类型的有机 C 含量低,O2 和 Eh 含量高,反硝化速率比另一种类型低 1000 倍,后者的有机 C 含量高,O2 和 Eh 含量低。潜在的硝化和反硝化速率与 Eh 呈负相关。这表明,在建立硝化或反硝化速率的采样方案之前,可以使用 Eh 来评估贫营养沉积物系统中反硝化菌和硝化菌种群的环境异质性。反硝化速率与硝化速率之间没有相关性,或者这两个过程与 NH4 (+) 或 NO3 (-) 浓度之间没有相关性。最大反硝化速率为 0.969 nmole N cm(-3) hour(-1),最大硝化速率为 23.6 nmole cm(-3) hour(-1),表明在这些贫营养沉积物中,硝化不会限制反硝化。一些沉积物岩芯的平均氧浓度为 6.0 mg/L,仍显示出硝化和反硝化活性。