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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, 1231–1241, 2013
https://doi.org/10.5194/bg-10-1231-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Nitrogen and global change

Biogeosciences, 10, 1231–1241, 2013
https://doi.org/10.5194/bg-10-1231-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 26 Feb 2013

Research article | 26 Feb 2013

Comparison of soil greenhouse gas fluxes from extensive and intensive grazing in a temperate maritime climate

U. Skiba1, S. K. Jones1,2, J. Drewer1, C. Helfter1, M. Anderson1, K. Dinsmore1, R. McKenzie1, E. Nemitz1, and M. A. Sutton1 U. Skiba et al.
  • 1Centre for Ecology and Hydrology, Bush Estate, Penicuik, Midlothian EH26 0QB, UK
  • 2Scotland's Rural College, West Mains Road, Edinburgh EH9 3JG, UK

Abstract. Greenhouse gas (GHG) fluxes from a seminatural, extensively sheep-grazed drained moorland and intensively sheep-grazed fertilised grassland in South East (SE) Scotland were compared over 4 yr (2007–2010). Nitrous oxide (N2O) and methane (CH4) fluxes were measured by static chambers, respiration from soil plus ground vegetation by a flow-through chamber, and the net ecosystem exchange (NEE) of carbon dioxide (CO2) by eddy-covariance. All GHG fluxes displayed high temporal and interannual variability. Temperature, radiation, water table height and precipitation could explain a significant percentage of seasonal and interannual variations. Greenhouse gas fluxes were dominated by the net ecosystem exchange of CO2 at both sites. Net ecosystem exchange of CO2 and respiration was much larger on the productive fertilised grassland (−1567 and 7157 g CO2eq m−2 yr−1, respectively) than on the seminatural moorland (−267 and 2554 g CO2eq m−2 yr−1, respectively). Large ruminant CH4 (147 g CO2eq m−2 yr−1) and soil N2O (384 g CO2eq m−2 yr−1) losses from the grazed grassland counteracted the CO2 uptake by 34%, whereas the small N2O (0.8 g CO2eq m−2 yr−1) and CH4 (7 g CO2eq m−2 yr−1) emissions from the moorland only impacted the NEE flux by 3%. The 4-yr average GHG budget for the grazed grassland was −1034 g CO2eq m−2 yr−1 and −260 g CO2eq m−2 yr−1 for the moorland.

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