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Isotopic constraints on atmospheric methane sources
If you have a question about this talk, please contact Dr Alex Archibald.
Carbon isotopic studies of atmospheric methane can provide constraints on the proportion of methane emitted to the atmosphere from different sources. At Royal Holloway δ13C in atmospheric methane is measured in samples from a network of sites in the Arctic, Atlantic and from Egham, SW of London.
The carbon isotopic signature of some major Arctic and sub-Arctic methane sources has been characterised from field studies. Methane from different sources has markedly different δ13C. Methane from northern wetlands has δ13C around -70‰; Siberian natural gas is around -50‰ and forest fire emissions are around around -28‰. Thus δ13C readily identifies specific source increments. The carbon isotopic signature of the bulk methane increment in ambient Arctic air has also been measured in air samples collected at the Zeppelin station, Spitsbergen. Results indicate a primarily biogenic source of methane to the Arctic in the summer months, most likely with a large wetland contribution.
This talk is part of the Centre for Atmospheric Science seminars, Chemistry Dept. series.
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Other listsWolfson College Lunchtime Seminar Series - Wednesdays of Full Term Cambridge Social Ontology Group (CSOG) Life Science Interface Seminars
Other talksDPMMS PhD student colloquium The Plight of Climate Refugees: Rising Seas, Melting Ice, and Inadequate Legal Protections "The Analysis of Recurrent Events: A Summary of Methodology and Informative Censoring Considerations" CERF in the City Professor Doug Winton - Title tbc Silicon cycling and opal production in the Atlantic: lessons from the last deglaciation