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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 4
Biogeosciences, 9, 1337–1350, 2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Understanding the impacts of hydrological changes on terrestrial...

Biogeosciences, 9, 1337–1350, 2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 12 Apr 2012

Research article | 12 Apr 2012

Nitrous oxide fluxes from tropical peat with different disturbance history and management

J. Jauhiainen1, H. Silvennoinen3,2, R. Hämäläinen2, K. Kusin4, S. Limin4, R. J. Raison5, and H. Vasander1 J. Jauhiainen et al.
  • 1University of Helsinki, Department of Forest Sciences, P.O. Box 27, 00014 University of Helsinki, Finland
  • 2University of Eastern Finland, Department of Environmental Sciences, P.O. Box 1627, Kuopio 70211, Finland
  • 3Norwegian University of Life Sciences, Department of Plant and Environmental Sciences, Fougnerbakken 3, 1432 Aas, Norway
  • 4University of Palangka Raya, CIMTROP, Palangka Raya 73112, Indonesia
  • 5CSIRO, Ecosystem Sciences, P.O. Box 1700, Canberra ACT 2601, Australia

Abstract. Tropical peatlands are one of the most important terrestrial ecosystems in terms of impact on the atmospheric greenhouse gas composition. Currently, greenhouse gas emissions from tropical peatlands following disturbances due to deforestation, drainage or wildfire are substantial. We quantified in situ nitrous oxide (N2O) fluxes during both dry and wet seasons using a closed chamber method at sites that represented differing land uses and land use change intensities in Central Kalimantan, Indonesia. Cumulative N2O fluxes were compared with carbon dioxide (CO2) and methane (CH4) fluxes.

The mean N2O flux rates (N2O-N ±: SD, mg m−2 h−1) varied as follows: drained forest (0.112 ± 0.293) > agricultural peat at the Kalampangan site (0.012 ± 0.026) > drained burned peat (0.011 ± 0.018) > agricultural peat at the Marang site (0.0072 ± 0.028) > undrained forest (0.0025 ± 0.053) > clear-felled, drained, recovering forest (0.0022 ± 0.021). The widest N2O flux range was detected in the drained forest (max. 2.312 and min. −0.043 mg N2O-N m−2 h−1). At the other flux monitoring sites the flux ranges remained at about one tenth that of the drained forest site. The highest N2O emission rates were observed at water tables close to the peat surface where also the flux range was widest. Annual cumulative peat surface N2O emissions (expressed in CO2 equivalents as a percentage of the total greenhouse gas (N2O, CO2 and CH4) emissions) were 9.2 % at highest, but typically ~1 %. Average N2O fluxes and also the total of monitored GHG emissions were highest in drainage-affected forest which is characterized by continuous labile nitrogen availability from vegetation, and water tables typically below the surface.

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