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Determinants of annual fluxes of CO2 and N2O in long-term no-tillage and conventional tillage systems in northern France
Authors:Katrien Oorts  Roel Merckx  Eric Grhan  Jrme Labreuche  Bernard Nicolardot
Institution:aINRA, Unité d’agronomie de Laon-Reims-Mons, 2 Esplanade Roland Garros, BP 224, 51686 Reims Cedex 2, France;bFaculty of Applied Bioscience and Engineering, Laboratory for Soil and Water Management, Kasteelpark Arenberg 20, 3001 Heverlee, Belgium;cINRA, Unité d’Agronomie de Laon-Reims-Mons, rue Fernand Christ, 02007 Laon Cedex, France;dARVALIS, Institut du végétal, Station Expérimentale, 91720 Boigneville, France
Abstract:The greenhouse gases CO2 and N2O emissions were quantified in a long-term experiment in northern France, in which no-till (NT) and conventional tillage (CT) had been differentiated during 32 years in plots under a maize–wheat rotation. Continuous CO2 and periodical N2O soil emission measurements were performed during two periods: under maize cultivation (April 2003–July 2003) and during the fallow period after wheat harvest (August 2003–March 2004). In order to document the dynamics and importance of these emissions, soil organic C and mineral N, residue decomposition, soil potential for CO2 emission and climatic data were measured. CO2 emissions were significantly larger in NT on 53% and in CT on 6% of the days. From April to July 2003 and from November 2003 to March 2004, the cumulated CO2 emissions did not differ significantly between CT and NT. However, the cumulated CO2 emissions from August to November 2003 were considerably larger for NT than for CT. Over the entire 331 days of measurement, CT and NT emitted 3160 ± 269 and 4064 ± 138 kg CO2-C ha−1, respectively. The differences in CO2 emissions in the two tillage systems resulted from the soil climatic conditions and the amounts and location of crop residues and SOM. A large proportion of the CO2 emissions in NT over the entire measurement period was probably due to the decomposition of old weathered residues. NT tended to emit more N2O than CT over the entire measurement period. However differences were statistically significant in only half of the cases due to important variability. N2O emissions were generally less than 5 g N ha−1 day−1, except for a few dates where emission increased up to 21 g N ha−1 day−1. These N2O fluxes represented 0.80 ± 0.15 and 1.32 ± 0.52 kg N2O-N ha−1 year−1 for CT and NT, respectively. Depending on the periods, a large part of the N2O emissions occurred was probably induced by nitrification, since soil conditions were not favorable for denitrification. Finally, for the period of measurement after 32 years of tillage treatments, the NT system emitted more greenhouses gases (CO2 and N2O) to the atmosphere on an annual basis than the CT system.
Keywords:Soil tillage  CO2 emission  N2O emission  Effect of climatic conditions  Crop residues  Soil organic matter
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