The application of NH 4 + -based fertilizers is a common practice in rice production. The immediate effect of a late season urea application on the processes involved in CH 4 emission from a rice field was investigated on sandy loam located in the valley of River Po at Vercelli, northern Italy, and planted with rice (Oryza sativa, type japonica, variety Koral). Urea, applied at a rate of 50kgNha - 1 on the 75th day after flooding, significantly stimulated both CH 4 production and CH 4 oxidation. During the following 9 days, the rates of CH 4 production and CH 4 oxidation in the 0-3cm soil layer increased by 24-52 and 18-41%, respectively, of the fertilized plot compared to the unfertilized control plot. Methane oxidation on roots was also stimulated by urea, indicated by shorter lag times. Porewater concentrations of CH 4 in the 0-6cm soil layer increased with time and soil depth, but were not affected by fertilization with urea. Urea application also exhibited little impact on CH 4 emission. During the 7 days following fertilization, urea only slightly reduced the CH 4 flux. Ammonium originating from urea hydrolysis was completely depleted from the porewater within 3 days, mainly due to plant uptake. Fertilizer application did also not affect the contribution of CH 4 oxidation to the net flux of CH 4 , determined by measuring δ 1 3 CH 4 and by inhibition of CH 4 oxidation. The absence of any effect of urea on net CH 4 emission in this study was presumably caused by the rapid depletion of urea, the counterbalance between the increase of CH 4 production and the increase of CH 4 oxidation after fertilization, and methanogenesis in deeper soil layers.