Stable carbon isotope signatures of methane from a Finnish subarctic wetland

Methane emissions from Lompolojänkkä, a Finnish aapa mire within the Arctic Circle, were studied by non-intrusive Keeling plot methods, to place better constraints on the seasonal variations in isotopic signature of methane (δ13CCH4) emitted from Arctic wetland. Air...

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Published in:Tellus B: Chemical and Physical Meteorology
Main Authors: S. Sriskantharajah, R. E. Fisher, D. Lowry, T. Aalto, J. Hatakka, M. Aurela, T. Laurila, A. Lohila, E. Kuitunen, E. G. Nisbet
Format: Article in Journal/Newspaper
Language:English
Published: Stockholm University Press 2012
Subjects:
Online Access:https://doi.org/10.3402/tellusb.v64i0.18818
https://doaj.org/article/41da41e51e624be881e07a9c5ff00d16
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spelling ftdoajarticles:oai:doaj.org/article:41da41e51e624be881e07a9c5ff00d16 2023-05-15T14:50:50+02:00 Stable carbon isotope signatures of methane from a Finnish subarctic wetland S. Sriskantharajah R. E. Fisher D. Lowry T. Aalto J. Hatakka M. Aurela T. Laurila A. Lohila E. Kuitunen E. G. Nisbet 2012-06-01T00:00:00Z https://doi.org/10.3402/tellusb.v64i0.18818 https://doaj.org/article/41da41e51e624be881e07a9c5ff00d16 EN eng Stockholm University Press http://www.tellusb.net/index.php/tellusb/article/view/18818/pdf_1 https://doaj.org/toc/0280-6509 https://doaj.org/toc/1600-0889 doi:10.3402/tellusb.v64i0.18818 0280-6509 1600-0889 https://doaj.org/article/41da41e51e624be881e07a9c5ff00d16 Tellus: Series B, Chemical and Physical Meteorology, Vol 64, Iss 0, Pp 1-8 (2012) Methane carbon isotopes Arctic wetland Finland greenhouse gas Meteorology. Climatology QC851-999 article 2012 ftdoajarticles https://doi.org/10.3402/tellusb.v64i0.18818 2022-12-30T23:54:13Z Methane emissions from Lompolojänkkä, a Finnish aapa mire within the Arctic Circle, were studied by non-intrusive Keeling plot methods, to place better constraints on the seasonal variations in isotopic signature of methane (δ13CCH4) emitted from Arctic wetland. Air samples were collected in Tedlar bags over the wetland at heights of 42 and 280 cm between May and October 2009 and in August 2008. The mixing ratio and δ13C of the methane in the samples were incorporated into Keeling plot analyses to derive bulk δ13CCH4 signatures for the methane inputs to the air above the wetland. The results show an unexpected consistence in δ13CCH4 from early to late summer, clustered around −68.5±0.7‰, but during spring thaw and autumnal freezing, δ13CCH4 is enriched by approximately 2 and 4‰, respectively. The techniques reported in this paper are simple and economical to employ, and give a bulk source signature for the methane inputs to the air above the entire wetland that can be extrapolated to a larger regional area. Article in Journal/Newspaper Arctic Subarctic Directory of Open Access Journals: DOAJ Articles Arctic Tellus B: Chemical and Physical Meteorology 64 1 18818
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Methane
carbon isotopes
Arctic wetland
Finland
greenhouse gas
Meteorology. Climatology
QC851-999
spellingShingle Methane
carbon isotopes
Arctic wetland
Finland
greenhouse gas
Meteorology. Climatology
QC851-999
S. Sriskantharajah
R. E. Fisher
D. Lowry
T. Aalto
J. Hatakka
M. Aurela
T. Laurila
A. Lohila
E. Kuitunen
E. G. Nisbet
Stable carbon isotope signatures of methane from a Finnish subarctic wetland
topic_facet Methane
carbon isotopes
Arctic wetland
Finland
greenhouse gas
Meteorology. Climatology
QC851-999
description Methane emissions from Lompolojänkkä, a Finnish aapa mire within the Arctic Circle, were studied by non-intrusive Keeling plot methods, to place better constraints on the seasonal variations in isotopic signature of methane (δ13CCH4) emitted from Arctic wetland. Air samples were collected in Tedlar bags over the wetland at heights of 42 and 280 cm between May and October 2009 and in August 2008. The mixing ratio and δ13C of the methane in the samples were incorporated into Keeling plot analyses to derive bulk δ13CCH4 signatures for the methane inputs to the air above the wetland. The results show an unexpected consistence in δ13CCH4 from early to late summer, clustered around −68.5±0.7‰, but during spring thaw and autumnal freezing, δ13CCH4 is enriched by approximately 2 and 4‰, respectively. The techniques reported in this paper are simple and economical to employ, and give a bulk source signature for the methane inputs to the air above the entire wetland that can be extrapolated to a larger regional area.
format Article in Journal/Newspaper
author S. Sriskantharajah
R. E. Fisher
D. Lowry
T. Aalto
J. Hatakka
M. Aurela
T. Laurila
A. Lohila
E. Kuitunen
E. G. Nisbet
author_facet S. Sriskantharajah
R. E. Fisher
D. Lowry
T. Aalto
J. Hatakka
M. Aurela
T. Laurila
A. Lohila
E. Kuitunen
E. G. Nisbet
author_sort S. Sriskantharajah
title Stable carbon isotope signatures of methane from a Finnish subarctic wetland
title_short Stable carbon isotope signatures of methane from a Finnish subarctic wetland
title_full Stable carbon isotope signatures of methane from a Finnish subarctic wetland
title_fullStr Stable carbon isotope signatures of methane from a Finnish subarctic wetland
title_full_unstemmed Stable carbon isotope signatures of methane from a Finnish subarctic wetland
title_sort stable carbon isotope signatures of methane from a finnish subarctic wetland
publisher Stockholm University Press
publishDate 2012
url https://doi.org/10.3402/tellusb.v64i0.18818
https://doaj.org/article/41da41e51e624be881e07a9c5ff00d16
geographic Arctic
geographic_facet Arctic
genre Arctic
Subarctic
genre_facet Arctic
Subarctic
op_source Tellus: Series B, Chemical and Physical Meteorology, Vol 64, Iss 0, Pp 1-8 (2012)
op_relation http://www.tellusb.net/index.php/tellusb/article/view/18818/pdf_1
https://doaj.org/toc/0280-6509
https://doaj.org/toc/1600-0889
doi:10.3402/tellusb.v64i0.18818
0280-6509
1600-0889
https://doaj.org/article/41da41e51e624be881e07a9c5ff00d16
op_doi https://doi.org/10.3402/tellusb.v64i0.18818
container_title Tellus B: Chemical and Physical Meteorology
container_volume 64
container_issue 1
container_start_page 18818
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