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Nitrous oxide (N 2 O) is one of the most prominent greenhouse gases that cause global warming and ozone layer depletion in the stratosphere (Ravishankara et al., 2009). Microbial production and consumption processes of N 2 O depend on soil physicochemical properties and climate condition (Frindte et al., 2019;Liao et al., 2020Liao et al., , 2021Wang et al., 2018). The global N 2 O fluxes are likely to respond rapidly to global climate change (e.g., increases in CO 2 and temperature and altered water availability), so it is critical to understand their feedback to climate change (

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