<p><strong>Abstract.</strong> This study reports NO, NO<sub>2</sub> and O<sub>3</sub> mixing ratios and flux measurements using the eddy-covariance method during a 7-months period over an oilseed rape field, spanning an organic and a mineral fertilisation event. Mean NO emissions during the whole period were in agreement with previous studies and showed quite small emissions of 0.26&#8201;kg&#8201;N&#8201;ha<sup>&#8722;1</sup> with an emission factor of 0.27&#8201;%, estimated as the ratio between total N emitted in form of NO and total N input. The NO emissions were higher following organic fertilisation in August due to conditions favouring nitrification (soil water content around 20&#8201;% and high temperatures), while mineral fertilisation in February did not result in large emissions. The ozone (O<sub>3</sub>) deposition velocity was significantly larger following organic fertilisation. We argue that reaction of O<sub>3</sub> with emitted NO or reaction of O<sub>3</sub> at the surface did not explain this finding, but we propose that reactions of O<sub>3</sub> with VOCs emitted by the slurry were the main reason. The analysis of the chemical and turbulent transport times showed that reactions between NO, NO<sub>2</sub> and O<sub>3</sub> below the measurement height occurred at all time during the 7-months period. Following organic fertilisation, the NO ground fluxes were 30&#8201;% larger than the NO fluxes at the measurement height (3.2&#8201;m) , while the NO<sub>2</sub> fluxes changed sign during some periods, being negative at the surface and positive at the measurement height. This phenomenon of "apparent NO<sub>2</sub> emissions" reveals to be important during strong NO emissions and high O<sub>3</sub> ambient mixing ratios, even on a bare soil during August.</p>