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甲烷代谢对受污染淡水沉积物中硝化和一氧化二氮产生的影响。

Effects of methane metabolism on nitrification and nitrous oxide production in polluted freshwater sediment.

机构信息

Microbiology Unit, Department of Natural Resource Sciences, Macdonald Campus of McGill University, Ste-Anne-de-Bellevue, Québec, Canada H9X 3V9.

出版信息

Appl Environ Microbiol. 1994 Sep;60(9):3307-14. doi: 10.1128/aem.60.9.3307-3314.1994.

Abstract

We report the effect of CH(4) and of CH(4) oxidation on nitrification in freshwater sediment from Hamilton Harbour, Ontario, Canada, a highly polluted ecosystem. Aerobic slurry experiments showed a high potential for aerobic N(2)O production in some sites. It was suppressed by C(2)H(2), correlated to NO(3) production, and stimulated by NH(4) concentration, supporting the hypothesis of a nitrification-dependent source for this N(2)O production. Diluted sediment slurries supplemented with CH(4) (1 to 24 muM) showed earlier and enhanced nitrification and N(2)O production compared with unsupplemented slurries (</=1 muM CH(4)). This suggests that nitrification by methanotrophs may be significant in freshwater sediment under certain conditions. Suppression of nitrification was observed at CH(4) concentrations of 84 muM and greater, possibly through competition for O(2) between methanotrophs and NH(4) -oxidizing bacteria and/or competition for mineral N between these two groups of organisms. In Hamilton Harbour sediment, the very high CH(4) concentrations (1.02 to 6.83 mM) which exist would probably suppress nitrification and favor NH(4) accumulation in the pore water. Indeed, NH(4) concentrations in Hamilton Harbour sediment are higher than those found in other lakes. We conclude that the impact of CH(4) metabolism on N cycling processes in freshwater ecosystems should be given more attention.

摘要

我们报告了加拿大安大略省汉密尔顿港淡水沉积物中 CH(4) 和 CH(4) 氧化对硝化作用的影响,该港是一个高度污染的生态系统。好氧泥浆实验表明,一些地点具有很高的好氧 N(2)O 产生潜力。它被 C(2)H(2) 抑制,与 NO(3) 产生相关,并受到 NH(4) 浓度的刺激,这支持了这种 N(2)O 产生源自硝化作用的假说。与未添加 CH(4) 的泥浆(<=1 muM CH(4))相比,添加了 CH(4)(1 至 24 muM)的稀释沉积物泥浆显示出更早和增强的硝化作用和 N(2)O 产生。这表明在某些条件下,甲烷营养菌的硝化作用可能在淡水沉积物中很重要。在 CH(4) 浓度为 84 muM 及更高时,观察到硝化作用受到抑制,这可能是由于甲烷营养菌和 NH(4) -氧化细菌之间对 O(2) 的竞争以及这两组生物之间对矿质氮的竞争所致。在汉密尔顿港沉积物中,存在的非常高的 CH(4) 浓度(1.02 至 6.83 mM)可能会抑制硝化作用并有利于 NH(4) 在孔隙水中积累。事实上,汉密尔顿港沉积物中的 NH(4) 浓度高于其他湖泊。我们得出结论,应更加关注 CH(4) 代谢对淡水生态系统氮循环过程的影响。

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