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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 10, issue 2
Biogeosciences, 10, 1083-1095, 2013
https://doi.org/10.5194/bg-10-1083-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Nitrogen and global change

Biogeosciences, 10, 1083-1095, 2013
https://doi.org/10.5194/bg-10-1083-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 15 Feb 2013

Research article | 15 Feb 2013

Nitrogen balance of a boreal Scots pine forest

J. F. J. Korhonen1, M. Pihlatie1, J. Pumpanen2, H. Aaltonen2, P. Hari2, J. Levula3, A.-J. Kieloaho1, E. Nikinmaa2, T. Vesala1, and H. Ilvesniemi4 J. F. J. Korhonen et al.
  • 1Department of Physics, University Of Helsinki, P.O. Box 48, 00014, Helsinki, Finland
  • 2Department of Forest Sciences, University Of Helsinki, P.O. Box 27, 00014, Helsinki, Finland
  • 3Hyytiälä Forestry Field station, Hyytiäläntie 124, 35500, Korkeakoski, Finland
  • 4Finnish Forest Research Institute, Vantaa Unit, P.O. Box 18, 01301, Vantaa, Finland

Abstract. The productivity of boreal forests is considered to be limited by low nitrogen (N) availability. Increased atmospheric N deposition has altered the functioning and N cycling of these N-sensitive ecosystems by increasing the availability of reactive nitrogen. The most important components of N pools and fluxes were measured in a boreal Scots pine stand in Hyytiälä, Southern Finland. The measurements at the site allowed direct estimations of nutrient pools in the soil and biomass, inputs from the atmosphere and outputs as drainage flow and gaseous losses from two micro-catchments. N was accumulating in the system, mainly in woody biomass, at a rate of 7 kg N ha−1 yr−1. Nitrogen input as atmospheric deposition was 7.4 kg N ha−1 yr−1. Dry deposition and organic N in wet deposition contributed over half of the inputs in deposition. Total outputs were 0.4 kg N ha−1 yr−1, the most important outputs being N2O emission to the atmosphere and organic N flux in drainage flow. Nitrogen uptake and retranslocation were equally important sources of N for plant growth. Most of the assimilated N originated from decomposition of organic matter, and the fraction of N that could originate directly from deposition was about 30%. In conclusion, atmospheric N deposition fertilizes the site considerably, but there are no signs of N saturation. Further research is needed to estimate soil N2 fluxes (emission and fixation), which may amount up to several kg N ha−1 yr−1.

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