ABSTRACT

Nitrous oxide (N₂O) reduction is a key process controlling and mitigating the highly heterogeneous N₂O emission from soils. We here developed a new method (¹⁵N₂O reduction tracing) to quantify potential gross reduction rates of N₂O by incubating only a few grams of soil samples, spiking single-labeled ¹⁵N₂O tracer as the direct substrate for N₂O reduction, and analyzing its direct product (the ¹⁵N/¹⁴N ratio of N₂). First, the mass balance between ¹⁵N₂O consumption and ¹⁵N₂ production was confirmed (recovery rate: 107% ± 10%) using pure cultures of complete denitrifying bacteria. Second, we tested our method’s applicability to soil profiles at a secondary forest (O, 0–5 cm A1, 5–20 cm A2 horizons), no-tillage agricultural plot (O, A1, A2), and conventional tillage plot (0–20 cm Ap horizon). Their N₂O reduction potentials under a controlled soil water potential (−1 kPa) and 0.1% ¹⁵N₂O air varied across orders of magnitude: higher in the shallower, carbon-rich horizons (O–A1). Our method allowed the direct comparison between the N₂O reductions and copy numbers of nosZ (the functional gene responsible for N₂O reduction), which revealed no clear relationship across the studied samples. Instead, the variation in N₂O reduction potential co-varied with the soil total carbon (C) content, C/N ratio, and 16S rRNA gene copy number, suggesting C substrate control on the N₂O reduction. By further reducing the required soil mass, the current method may help to identify N₂O reduction hotspots at smaller scales and clarify mechanisms behind the heterogenous N₂O dynamics in soils.