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Nitrifier denitrification can be a source of N2O from soil: a revised approach to the dual‐isotope labelling method

反硝化 土壤水分 一氧化二氮 化学 环境化学 氮同位素 环境科学 氮气 土壤科学 有机化学
作者
Dorien M. Kool,N. Wrage,Sophie Zechmeister‐Boltenstern,M. Pfeffer,D.J. Brus,O. Oenema,Jan Willem van Groenigen
出处
期刊:European Journal of Soil Science [Wiley]
卷期号:61 (5): 759-772 被引量:152
标识
DOI:10.1111/j.1365-2389.2010.01270.x
摘要

Nitrifier denitrification (i.e. nitrite reduction by ammonia oxidizers) is one of the biochemical pathways of nitrous oxide (N 2 O) production. It is increasingly suggested that this pathway may contribute substantially to N 2 O production in soil, the major source of this greenhouse gas. However, although monoculture studies recognize its potential, methodological drawbacks prohibit conclusive proof that nitrifier denitrification occurs in actual soils. Here we suggest and apply a new isotopic approach to identify its presence in soil. In incubation experiments with 12 soils, N 2 O production was studied using oxygen (O) and nitrogen (N) isotope tracing, accounting for O exchange. Microbial biomass C and N and phospholipid fatty acid (PLFA) patterns were analysed to explain potential differences in N 2 O production pathways. We found that in at least five of the soils nitrifier denitrification must have contributed to N 2 O production. Moreover, it may even have been responsible for all NH 4 + ‐derived N 2 O in most soils. In contrast, N 2 O as a by‐product of ammonia oxidation contributed very little to total production. Microbial biomass C and N and PLFA‐distinguished microbial community composition were not indicative of differences in N 2 O production pathways. Overall, we show that combined O and N isotope tracing may still provide a powerful tool to understand N 2 O production pathways, provided that O exchange is accounted for. We conclude that nitrifier denitrification can indeed occur in soils, and may in fact be responsible for the greater proportion of total nitrifier‐induced N 2 O production.
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