Abstract

Fertilized agricultural soils are a significant source of NO, a gas involved in tropospheric ozone formation. The aims of the research reported here were to measure NO fluxes over the length of the growing season of wheat and maize crops, and to build a model of soil NO emissions from arable land. Field experiments were carried out on a 1-ha field divided into two parts. The first one was cropped with wheat and harvested in late July, 2002, whereas the second part was sown with maize and harvested in October. The wheat and maize received 130 kg N ha−1 and 140 kg N ha−1, respectively. For each crop, NO fluxes were measured during 10 months every 2 weeks using manual closed chambers, and continuously with a wind tunnel immediately after nitrogen fertilization. Fertilizer application significantly affected NO emissions: the largest NO emissions were recorded a few days after nitrogen application. This delay depended on the kinetics of nitrogen incorporation in the soil, as influenced by rainfall. The emissions measured on the maize field (2.6% of the fertilizer amount applied) were more important than those on the wheat field (1.0% of the fertilizer amount applied), owing to differences in timing of nitrogen application, with respect to climate and crop growth. Relationships between soil nitrification rate and NO emission obtained from laboratory incubations, and experimental data appeared useful and relevant to predict NO emissions at the field-scale.

Highlights

  • Nitrogen oxides (NOx=nitric oxide (NO)+NO2) play a central role in the tropospheric photochemistry leading to ozone formation

  • NO emissions under wheat were higher after the second fertilization compared to the first one, despite the nitrogen input to the soil being only effective 3 weeks after application

  • Our measurements highlighted a large dependence of NO emissions on mineral nitrogen fertilization: emissions were largest during the few days following nitrogen inputs, with mean daily rates greater than 300 g N haÀ1 dayÀ1

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Summary

Introduction

Nitrogen oxides (NOx=NO+NO2) play a central role in the tropospheric photochemistry leading to ozone formation. In terms of global source strength, biogenic emissions from soils are highly uncertain, with global estimates ranging between 5.5 and 21 Tg N (Yienger and Levy 1995; Davidson 1991), and accounting for up to 40% of the global NOx budget (Davidson and Kingerlee 1997). With predicted increases in N fertilizer use, the agricultural source of atmospheric NOx is likely to increase and to contribute to more than 50% of the global soil emissions in the future (Yienger and Levy 1995). Nitric oxide is a direct intermediate of the denitrification pathway, and its net release is greatly influenced by its gas phase diffusivity in the soil, and its consumption by denitrifiers. Ammonium-based fertilizers increase NO emissions both by stimulating NO production by nitrification, and by decreasing NO consumption

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