资源环境科技发展态势分析平台

Nitrous oxide (N₂O) is a potent ozone-depleting greenhouse gas produced by incomplete denitrification. Recent works on riverine N₂O emissions focus mainly on contributions from in-channel, benthic, and fluvial hyporheic environments under assumptions of steady-state conditions and homogeneous sediment hydraulic conductivity (K). However, riparian floodplains are also a potentially important N₂O source characterized by complex sediment heterogeneity and dynamic surface and groundwater interactions. We use numerical flow and reactive transport models to investigate the influence of complex sedimentary architecture and high-flow events (e.g., storms) on N₂O production. We interpret the correlation between flow and solute fields with the flow topological Okubo-Weiss metric (OW) and the scalar dissipation rate weighted by soil organic matter fraction and soil saturation. We model a heterogeneous riparian floodplain based on field observations from the Theis Environmental Monitoring and Modeling Site, Ohio, USA. N₂O production is greatest within intermediate-K sediments (e.g., sands) where denitrification rates are highest, and emissions increase by more than an order of magnitude during storms. Sensitivity analysis reveals that the denitrification rate is most influential for N₂O flux, accounting for nearly 46% of the variance in production rates. Denitrification rates adapt to spatial changes in the flow topology (measured by OW) related to sediment heterogeneity and are strongly influenced by subsurface mixing dynamics. Mixing is greatest in shear strain-dominated regions, while vorticity promotes OM dissolution and prolongs residence times. Accurate lithologic representation is imperative for characterizing subsurface N₂O production dynamics, especially given growing concern regarding climate change driven hydrologic changes within watersheds worldwide.

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