Isotopologue enrichment factors of N2O reduction in soils

Isotopic signatures can be used to study sink and source processes of N₂O, but the success of this approach is limited by insufficient knowledge on the isotope fractionation factors of the various reaction pathways. We investigated isotope enrichment factors of the N₂O‐to‐N₂ step of denitrification (ε) in two arable soils, a silt‐loam Haplic Luvisol and a sandy Gleyic Podzol. In addition to the ε of ¹⁸O (ε_18O) and of average ¹⁵N (ε_bulk), the ε of the ¹⁵N site preference within the linear N₂O molecule (ε_SP) was also determined. Soils were anaerobically incubated in gas‐tight bottles with N₂O added to the headspace to induce N₂O reduction. Pre‐treatment included the removal of NO to prevent N₂O production. Gas samples were collected regularly to determine the dynamics of N₂O reduction, the time course of the isotopic signatures of residual N₂O, and the associated isotope enrichment factors. To vary reduction rates and associated fractionation factors, several treatments were established including two levels of initial N₂O concentration and anaerobic pre‐incubation with or without addition of N₂O. N₂O reduction rates were affected by the soil type and initial N₂O concentration. The ε_18O and ε_bulk ranged between ?13 and ?20‰, and between ?5 and ?9‰, respectively. Both quantities were more negative in the Gleyic Podzol. The ε of the central N position (ε_α) was always larger than that of the peripheral N‐position (ε_β), giving ε_SP of ?4 to ?8‰. The ranges and variation patterns of ε were comparable with those from previous static incubation studies with soils. Moreover, we found a relatively constant ratio between ε_18O and ε_bulk which is close to the default ratio of 2.5 that had been previously suggested. The fact that different soils exhibited comparable ε under certain conditions suggests that these values could serve to identify N₂O reduction from the isotopic fingerprints of N₂O emitted from any soil. Copyright © 2009 John Wiley & Sons, Ltd.