Reactive oxygen species (ROS)-induced element/pollutant geochemical processes in fluctuating anoxic-oxic areas have received increasing attention in recent years. Nitrous oxide (N2O) is a strong greenhouse gas; however, the relationship between ROS and N2O emissions in these areas has not been established. This work revealed the essential role of ROS in promoting N2O emissions in soil/sediment during the anoxic-oxic transition. ROS decreased the rate of nitrate reduction by 26-31% and increased N2O emissions by 8.8-31.3% (at 48 h). ROS-induced N2O emission was via inhibiting the step of N2O reduction. During the anoxic-oxic transition, the contribution of ROS to inhibit the step of N2O reduction was higher than 52.6%, demonstrating the important role of ROS. The downregulated relative transcription of the NosZ gene demonstrated inhibition at the gene level. Hydrogen peroxide was the dominant ROS species inhibiting N2O reduction, while the role of hydroxyl radicals was negligible, suggesting a different behavior of N2O emission with common pollutant conversion induced by ROS during the anoxic-oxic transition. This study demonstrated an overlooked factor in promoting N2O emission in the soil/sediment and appealed to a re-examination of the mechanism of N2O emissions in fluctuating anoxic-oxic areas.
Keywords: anoxic−oxic transition; denitrification; nitrous oxide; reactive oxygen species; sediment; soil.