摘要：Paddy fields are significant anthropogenic sources of methane (CH<sub>4</sub>) emissions. In southern Brazil, rice is grown in lowland flooded areas once a year, followed by a long fallow period. This study aimed to measure CH<sub>4</sub> fluxes in a rice paddy field in southern Brazil during the rice-growing season of 2015/2016 and the following fallow period. The fluxes were estimated using the eddy covariance (EC) technique and soil chamber (SC). Diurnal and seasonal variations of CH<sub>4</sub> fluxes and potential meteorological drivers were analyzed. The CH<sub>4</sub> fluxes showed distinct diurnal variations in each analyzed subperiod (vegetative, reproductive, pre-harvest, no rice, and land preparation), characterized by a single-peak diurnal pattern. The variables that most influenced methane emissions were air and surface temperatures. In the growing season, the rice vegetative stage was responsible for most of the measured emissions. The accumulated annual emission estimated was 44.88 g CH<sub>4</sub> m<sup>−2</sup> y<sup>−1</sup>, being 64% (28.50 g CH<sub>4</sub> m<sup>−2</sup>) due to the rice-growing season and 36% (16.38 g CH<sub>4</sub> m<sup>−2</sup>) due to the fallow period. These results show the importance of including fallow periods in strategies to mitigate methane emissions in flood irrigated rice-growing areas.
