Increasing levels of atmospheric CO are expected to enhance crop yields and alter soil greenhouse gas fluxes from rice paddies. While elevated CO ( ) effects on CH emissions from rice paddies have been studied in some detail, little is known how might affect N O fluxes or yield-scaled emissions. Here, we report on a multi-site, multi-year in-situ FACE (free-air CO enrichment) study, aiming to determine N O fluxes and crop yields from Chinese subtropical rice systems as affected by . In this study, we tested various N fertilization and residue addition treatments, with rice being grown under either (+200 μmol/mol) or ambient control. Across the six site-years, rice straw and grain yields under were increased by 9%-40% for treatments fertilized with ≥150 kg N/ha, while seasonal N O emissions were decreased by 23%-73%. Consequently, yield-scaled N O emissions were significantly lower under . For treatments receiving insufficient fertilization (≤125 kg N/ha), however, no significant effects on N O emissions were observed. The mitigating effect of upon N O emissions is closely associated with plant N uptake and a reduction of soil N availability. Nevertheless, increases in yield-scaled N O emissions with increasing N surplus suggests that N surplus is a useful indicator for assessing N O emissions from rice paddies. Our findings indicate that with rising atmospheric CO soil N O emissions from rice paddies will decrease, given that the farmers' N fertilization is usually sufficient for crop growth. The expected decrease in N O emissions was calculated to compensate 24% of the simultaneously observed increase in CH emissions under . This shows that for an agronomic and environmental assessment of effects on rice systems, not only CH emissions, but also N O fluxes and yield-scaled emissions need to be considered for identifying most climate-friendly and economically viable options for future rice production.

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http://dx.doi.org/10.1111/gcb.15410DOI Listing

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