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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 3, issue 2
Biogeosciences, 3, 135-145, 2006
https://doi.org/10.5194/bg-3-135-2006
© Author(s) 2006. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

Special issue: Nitrogen oxides (NO, NO2, N2O) emissions...

Biogeosciences, 3, 135-145, 2006
https://doi.org/10.5194/bg-3-135-2006
© Author(s) 2006. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  20 Mar 2006

20 Mar 2006

Sources of nitrous oxide emitted from European forest soils

P. Ambus1, S. Zechmeister-Boltenstern2, and K. Butterbach-Bahl3 P. Ambus et al.
  • 1Risø National Laboratory, Biosystems Department (BIO-309), 4000 Roskilde, Denmark
  • 2Federal Research and Training Centre for Forests, Natural Hazards and Landscape (BFW), Vienna, Austria
  • 3Karlsruhe Research Centre, Institute for Meteorology and Climate Research, Atmospheric Environmental Research (IMK-IFU), Garmisch-Partenkirchen, Germany

Abstract. Forest ecosystems may provide strong sources of nitrous oxide (N2O), which is important for atmospheric chemical and radiative properties. Nonetheless, our understanding of controls on forest N2O emissions is insufficient to narrow current flux estimates, which still are associated with great uncertainties. In this study, we have investigated the quantitative and qualitative relationships between N-cycling and N2O production in European forests in order to evaluate the importance of nitrification and denitrification for N2O production. Soil samples were collected in 11 different sites characterized by variable climatic regimes and forest types. Soil N-cycling and associated production of N2O was assessed following application of 15N-labeled nitrogen. The N2O emission varied significantly among the different forest soils, and was inversely correlated to the soil C:N ratio. The N2O emissions were significantly higher from the deciduous soils (13 ng N2O-N cm-3 d-1) than from the coniferous soils (4 ng N2O-N cm-3 d-1). Nitrate (NO3-) was the dominant substrate for N2O with an average contribution of 62% and exceeding 50% at least once for all sites. The average contribution of ammonium (NH4+) to N2O averaged 34%. The N2O emissions were correlated with gross nitrification activities, and as for N2O, gross nitrification was also higher in deciduous soils (3.4 µg N cm-3 d-1) than in coniferous soils (1.1 µg N cm-3 d-1). The ratio between N2O production and gross nitrification averaged 0.67% (deciduous) and 0.44% (coniferous). Our study suggests that changes in forest composition in response to land use activities and global change may have implications for regional budgets of greenhouse gases. From the study it also became clear that N2O emissions were driven by the nitrification activity, although the N2O was produced per se mainly from denitrification. Increased nitrification in response to accelerated N inputs predicted for forest ecosystems in Europe may thus lead to increased greenhouse gas emissions from forest ecosystems.

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