Total hydrocarbon flux dynamics at a subarctic mire in northern Sweden
Stockholm University, Faculty of Science, Department of Geology and Geochemistry2008 (English)In: Journal of Geophysical Research – Biogeosciences, Vol. 113, G03026- p.Article in journal (Refereed) Published
This is a study of the spatial and temporal variability of total hydrocarbon (THC) emissions from vegetation and soil at a subarctic mire, northern Sweden. THCs include methane (CH4) and nonmethane volatile organic compounds (NMVOCs), both of which are atmospherically important trace gases and constitute a significant proportion of the carbon exchange between biosphere and atmosphere. Reliable characterization of the magnitude and the dynamics of the THC fluxes from high latitude peatlands are important when considering to what extent trace gas emissions from such ecosystems may change and feed back on climate regulation as a result of warmer climate and melting permafrost. High frequency measurements of THC and carbon dioxide (CO2) were conducted during four sequential growing seasons in three localities representing the trophic range of plant communities at the mire. The magnitude of the THC flux followed the moisture gradient with increasing emissions from a dry Palsa site (2.2 ± 0.1 mgC m−2 d−1), to a wet intermediate melt feature with Sphagnum spp. (28 ± 0.3 mgC m−2 d−1) and highest emissions from a wet Eriophorum spp. site (122 ± 1.4 mgC m−2 d−1) (overall mean ±1 SE, n = 2254, 2231 and 2137). At the Palsa site, daytime THC flux was most strongly related to air temperature while daytime THC emissions at the Sphagnum site had a stronger relation to ground temperature. THC emissions at both the wet sites were correlated to net ecosystem exchange of CO2. An overall spatial correlation indicated that areas with highly productive vegetation communities also had high THC emission potential.
Place, publisher, year, edition, pages
2008. Vol. 113, G03026- p.
Earth and Related Environmental Sciences
IdentifiersURN: urn:nbn:se:su:diva-25513DOI: 10.1029/2008JG000703ISI: 000258822700001OAI: oai:DiVA.org:su-25513DiVA: diva2:199878
Part of urn:nbn:se:su:diva-82412008-10-092008-10-012012-03-26Bibliographically approved