Wildfire alters nitrogen cycling to increase soil emissions of nitric oxide (NO) and the heterogeneity of nitrous oxide (N2O) in California chaparral

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Authors: Elizah Z. Stephens, M. Fabiola Pulido Barriga, Aral C. Greene, Alexander H. Krichels, Meg Kargul, Loralee Larios, Sydney I. Glassman, Peter M. Homyak
Cited by: 1
References: 74

Abstract

Abstract Wildfires can disrupt ecosystem nitrogen (N) cycling by combusting vegetation biomass N and depositing ash that is rich in ammonium (NH 4 + ) onto soils. Post-fire increases in NH 4 + and soil physicochemical changes may promote further N loss by stimulating microbially-driven emissions of nitric oxide (NO) and nitrous oxide (N 2 O)—trace gases that alter air quality and climate. We hypothesized that soil NO and N 2 O emissions would increase with the flush of post-fire N availability and would be highest in soils that burned at medium severity due to the combination of high soil N availability and persistence of microbial activity. To test this, we established nine plots (6 burned; 3 unburned) and sampled soils seasonally over three years after wildfire in a chaparral shrubland in Southern California, USA. Wildfire significantly increased soil extractable NH 4 + by an average of 10 µg NH 4 + -N g soil -1 , soil extractable NO 3 - by 8 µg NO 3 - -N, and soil pH by 0.5 units. Post-fire soil NO emissions significantly increased by an average 74 ng NO-N g -1 (cumulative 40-h incubations) over three years, with the highest emissions measured in year one from plots that burned at medium and high severities. No significant effects of burning were detectable for N 2 O emissions over three years (average ± standard error; 224 ± 107 ng N 2 O-N g -1 soil in burned plots and 30 ± 17 ng N 2 O-N g -1 soil in unburned plots); however, we observed high fluxes only from soils that burned at medium and high severities (N 2 O > 3500 ng N 2 O-N g -1 soil). Isotopic characterization of N 2 O from high-emitting soils indicated contributions from diverse sources and increased N 2 O reduction to N 2 . Overall, the occurrence of high N 2 O fluxes and accelerated NO emissions post fire indicate wildfires interact with soil N cycling to promote burn-severity-sensitive gaseous N losses long after wildfires are extinguished.

Fields of Study & Subjects

Soil Carbon and Nitrogen Dynamics Groundwater and Isotope Geochemistry Fire effects on ecosystems

Publication details

Journal / source
Geoderma
Publisher
Elsevier BV
Volume
469
Pages
117807–117807
Publication date
11 April 2026
Language
EN