Comparison of greenhouse gas fluxes and nitrogen budgets from an ombotrophic bog in Scotland and a minerotrophic sedge fen in Finland

European Journal of Soil Science - Tập 61 Số 5 - Trang 640-650 - 2010
Julia Drewer1, Annalea Lohila2, Mika Aurela2, Tuomas Laurila2, Kari Minkkinen3, Timo Penttilä4, Kerry J. Dinsmore1, Rebecca McKenzie1, Carole Helfter1, Christophe Fléchard5, Mark A. Sutton1, U. Skiba1
1Centre for Ecology and Hydrology, Bush Estate, Penicuik EH26 0QB, UK
2Finnish Meteorological Institute, Climate Change Research, FI-00101 Helsinki, Finland
3Department of Forest Ecology, Peatland Ecology Group, University of Helsinki, FI-00014 Helsinki, Finland
4Vantaa Research Unit, Finnish Forest Research Institute, FI-01301 Vantaa, Finland
5Soils, Agronomy and Spatialization (SAS) Unit, INRA, 65 rue de St-Brieuc, 35042 Rennes Cedex, France

Tóm tắt

Northern peatlands cover approximately 4% of the global land surface area. Those peatlands will be particularly vulnerable to environmental and climate change and therefore it is important to investigate their total greenhouse gas (GHG) budgets, to determine the feedback on the climate. Nitrogen (N) is known to influence the GHG budget in particular by affecting the methane (CH4) balance. At two peatland sites in Scotland and Finland GHG fluxes of carbon dioxide (CO2), methane and nitrous oxide (N2O) and nitrogen fluxes were measured as part of the European project ‘NitroEurope’. The Scottish site, Auchencorth Moss, was a GHG sink of −321, −490 and −321 g CO2 eq m−2 year−1 in 2006, 2007 and 2008, respectively, with CO2 as the dominating GHG. In contrast, the dominating GHG at the Finnish site, Lompolojänkkä, was CH4, resulting in the site being a net GHG source of +485 and +431 g CO2 eq m−2 year−1 in 2006 and 2007, respectively. Therefore, Auchencorth Moss had a negative global warming potential (GWP) whilst Lompolojänkkä had a positive GWP over the investigated time period. Initial results yielded a positive N budget for Lompolojänkkä of 7.1 kg N ha−1 year−1, meaning the site was gaining nitrogen, and a negative N budget for Auchencorth Moss of −2.4 kg N ha year−1, meaning the site was losing nitrogen.

Từ khóa


Tài liệu tham khảo

10.2307/2260396

Aurela M., 2004, Research Unit on Physics, Chemistry and Biology of Atmospheric Composition and Climate Change: III Progress Report and Proceedings of Seminar in Pallas 29.3.‐1.4.2005, 28

Aurela M., 2009, Carbon dioxide exchange on a northern boreal fen., Boreal Environment Research, 14, 699

10.1016/0045-6535(93)90427-7

10.1029/2003GB002058

Bleeker A. Reinds G.J. Vermeulen A.T. De Vries W.&Erisman J.W.2004.Critical Loads and Present Deposition Thresholds of Nitrogen and Acidity and Their Exceedances at the Level II and Level I Monitoring Plots in Europe.ECN report ECN‐C–04‐117 Energy Research Centre of the Netherlands Petten December 2004.

10.1016/S0168-6496(03)00304-0

10.1029/94JD00218

Davidson E.A., 1991, Microbial Production and Consumption of Greenhouse Gases: Methane, Nitrogen Oxides and Halomethanes, 219

Denman K.L., 2007, Climate Change 2007: The Physical Science Basis., 499

10.1016/j.soilbio.2009.03.022

10.1111/j.1365-2486.2009.02119.x

10.1016/1352-2310(94)90433-2

Fowler D. Flechard C.R. Milford C. Hargreaves K.J. Storeton‐West R.L. Nemitz E.et al.1996.Towards Development of a Deposition Monitoring Network for Air Pollution in Europe: Measurements of Pollutant Concentrations and Deposition Fluxes to Moorland at Auchencorth Moss in Southern Scotland 1995.LIFE project report 93/NL/A32/ NL/3547 CEC Brussels.

10.1111/j.1365-2486.2007.01339.x

10.2307/1941811

10.1890/0012-9658(2001)082[1982:EOTANA]2.0.CO;2

10.1016/S1352-2310(98)00082-X

10.1007/s007040170015

Hatakka J., 2003, Overview of the atmospheric research activities and results at Pallas GAW station., Boreal Environment Research, 8, 365

10.1002/(SICI)1099-1085(19970315)11:3<325::AID-HYP476>3.0.CO;2-I

Huttunen J.T., 2002, Fluxes of nitrous oxide on natural peatlands in Vuotos, an area projected for a hydroelectric reservoir in northern Finland., Suo, 53, 87

10.1016/S1352-2310(02)00771-9

10.1016/j.tree.2006.06.004

10.1007/s11104-007-9374-6

Lappalainen E., 1996, Global Peat Resources.

Livingston G.P., 1995, Biogenic Trace Gases: Measuring Emissions from Soil and Water, 14

10.1111/j.1365-2389.2010.01265.x

10.1007/BF00000898

10.1016/S1352-2310(97)00265-3

10.1016/j.scitotenv.2008.03.015

10.1111/j.1365-2486.2004.00882.x

Mustajärvi K., 2008, Fluxes of dissolved organic and inorganic nitrogen in relation to stand characteristics and latitude in Scots pine and Norway spruce stands in Finland., Boreal Environment Research, 13, 3

10.1023/A:1006452609284

10.1016/j.agrformet.2003.12.001

10.1007/BF02183033

10.1111/j.1365-2486.2005.001002.x

10.1111/j.1600-0889.2007.00261.x

Saarnio S., 2007, Annual CO2 and CH4 fluxes of pristine boreal mires as a background for the lifecycle analyses of peat energy., Boreal Environment Research, 12, 101

10.1016/B978-0-12-639010-0.50007-8

Skiba U., 2000, The control of nitrous oxide emissions from agricultural and natural soils., Chemosphere, 2, 379

10.1016/j.agee.2009.05.018

10.1016/S1352-2310(99)00517-8

Sutton M.A., 2001, A new diffusion denuder system for long‐term, regional monitoring of atmospheric ammonia and ammonium., WASP Focus, 1, 145

10.1016/j.envpol.2007.04.014

10.1016/j.agrformet.2006.03.022

10.1016/j.agee.2009.04.027

10.1191/0959683602hl522rp

10.1029/2003GB002154

10.1023/A:1015798428743