Quantifying N 2 O reduction to N 2 based on N 2 O isotopocules – validation with independent methods (helium incubation and 15 N gas flux method)
Stable isotopic analyses of soil-emitted N2O (δ15Nbulk, δ18O and δ15Nsp = 15N site preference within the linear N2O molecule) may help to quantify N2O reduction to N2, an important but rarely quantified process in the soil nitrogen cycle. The N2O residual fraction (remaining unreduced N2O, rN2O) can...
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Published in | Biogeosciences Vol. 14; no. 3; pp. 711 - 732 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
14.02.2017
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Online Access | Get full text |
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