Soil nitrous oxide and methane fluxes are low from a bioenergy crop (canola) grown in a semi‐arid climate

Understanding nitrous oxide (N 2 O) and methane (CH 4 ) fluxes from agricultural soils in semi‐arid climates is necessary to fully assess greenhouse gas emissions from bioenergy cropping systems, and to improve our knowledge of global terrestrial gaseous exchange. Canola is grown globally as a feedstock for biodiesel production, however, resulting soil greenhouse gas fluxes are rarely reported for semi‐arid climates. We measured soil N 2 O and CH 4 fluxes from a rain‐fed canola crop in a semi‐arid region of south‐western Australia for 1 year on a subdaily basis. The site included N fertilized (75 kg N ha −1  yr −1 ) and nonfertilized plots. Daily N 2 O fluxes were low (−1.5 to 4.7 g N 2 O‐N ha −1  day −1 ) and culminated in an annual loss of 128 g N 2 O‐N ha −1 (standard error, 12 g N 2 O‐N ha −1 ) from N fertilized soil and 80 g N 2 O‐N ha −1 (standard error, 11 g N 2 O‐N ha −1 ) from nonfertilized soil. Daily CH 4 fluxes were also low (−10.3 to 11.9 g CH 4 ‐C ha −1  day −1 ), and did not differ with treatments, with an average annual net emission of 6.7 g CH 4 –C ha −1 (standard error, 20 g CH 4 –C ha −1 ). Greatest daily N 2 O fluxes occurred when the soil was fallow, and following a series of summer rainfall events. Summer rainfall increased soil water contents and available N, and occurred when soil temperatures were >25 °C, and when there was no active plant growth to compete with soil microorganisms for mineralized N; conditions known to promote N 2 O production. The proportion of N fertilizer emitted as N 2 O, after correction for emissions from the no N fertilizer treatment, was 0.06%; 17 times lower than IPCC default value for the application of synthetic N fertilizers to land (1.0%). Soil greenhouse gas fluxes from bioenergy crop production in semi‐arid regions are likely to have less influence on the net global warming potential of biofuel production than in temperate climates.