The Isotopic Composition of Atmospheric Methane and Its Sources

2000 ◽  
pp. 25-41 ◽  
Author(s):  
C. M. Stevens ◽  
M. Wahlen
1991 ◽  
Vol 96 (D8) ◽  
pp. 15455 ◽  
Author(s):  
David C. Lowe ◽  
Carl A. M. Brenninkmeijer ◽  
Stanley C. Tyler ◽  
Edward J. Dlugkencky

2020 ◽  
Author(s):  
Mila Stanisavljevic ◽  
Jaroslaw Nęcki ◽  
Piotr Korbeń ◽  
Hossein Maazallahi ◽  
Malika Menoud ◽  
...  

<p>Atmospheric methane is the second most important anthropogenic greenhouse gas after carbon dioxide. On the global scale, methane emissions are reasonably well constrained but the contributions from individual sources are highly uncertain (Saunois, 2016). According to bottom-up estimates, methane emissions from underground coal mining excavation contribute 11% to all anthropogenic methane sources (Saunois, 2016). However, there is a lack of in situ measurement to verify these estimates. Here we present results from measurements of the methane mole fraction over the Polish part of the Upper Silesian Coal Basin (USCB). Methane mole fraction was measured using vehicles equipped with high precision laser-based instruments (Picarro G2201-i CRDS, Picarro G2301- CRDS). Basic meteorological data (wind speed, wind direction) and GPS location data were collected on the roof of the vehicles. In order to obtain emission estimates, we attempted to cross the plumes from the coal mine shafts using public roads approximately perpendicular to plume downwind from the source. When possible, the plumes were intersected several times at different distances in order to have a closer look at uncertainties. A Gaussian plume model was used to calculate the release rate from the methane single source.</p><p>In addition to methane mole fraction measurements, we collected air samples for isotopic characterization (δ<sup>13</sup>C and δD) using isotope ratio mass spectrometry. We observed significant variation in measured methane isotopic composition over USCB (the results are in a range of -321 to -142 ‰ SMOW for δD and -31 to -58 ‰ VPDB for δ<sup>13</sup>CH<sub>4</sub>). The results indicated a much larger variability of the isotopic composition of methane emitted from coal mines than assumed previously, which may complicate the distinction of methane emissions from different sources by isotopic characterization.</p><p><strong>Keywords</strong>: Methane, Greenhouse Gases, Clime Change, Coal Mine Ventilation Shafts, Methane Isotopic Compositions</p><p>Reference:</p><p>Saunois, M., Bousquet, P., Poulter, B., et al., 2016a. The global methane budget, 2000–2012. Earth Syst. Sci. Data 8, 697–751. https://doi.org/10.5194/essd-8-697-2016. www.earth-syst-sci-data.net/8/697/2016/.</p><p>This work is part of the Marie Sklodowska-Curie Initial Training Network MEMO2 , which enable us to extend these measurements to other European locations</p>


1988 ◽  
Vol 2 (4) ◽  
pp. 385-397 ◽  
Author(s):  
Paul D. Quay ◽  
Stagg L. King ◽  
John M. Lansdown ◽  
David O. Wilbur

2020 ◽  
Author(s):  
Rebecca Fisher ◽  
Euan Nisbet ◽  
James France ◽  
Amber Riddle ◽  
David Lowry ◽  
...  

<p>Emissions of methane from combustion sources are typically distinguished by being enriched in <sup>13</sup>C and <sup>2</sup>H, causing a large isotopic shift to atmospheric methane δ<sup>13</sup>C and δD measurements downwind of fires.</p><p>The isotopic composition of the plant material being burnt has a strong effect on the isotopic composition of methane, with combustion of C4 plant material producing methane more enriched in <sup>13</sup>C than C3 plant combustion. Characterisation of the bulk isotopic signature of methane emitted from large areas of biomass burning is required to improve our ability to use isotopes in global models and ascertain the extent to which fire emissions influence interannual variations in the methane budget.</p><p>Two approaches have been used to collect air samples from large areas of biomass burning for isotopic characterisation of methane emitted from the fires. In campaigns in Senegal, Uganda, Zambia and Finland, the UK’s FAAM research aircraft flew through fire plumes and onboard measurement of methane concentration allowed targeted sampling within the plumes. This work was carried out as part of the NERC highlight Global Methane Budget project (MOYA). Ground based sampling downwind of fires around Sydney, New South Wales in late 2019/early 2020 has allowed isotopic characterisation of those plumes. All air samples were measured by isotope ratio mass spectrometry at Royal Holloway University of London and Keeling plots used to identify source signatures, e.g. δ<sup>13</sup>C for fires in Senegal in March 2017 was -28.5 ± 0,8 , typical of C3 burning.</p><p>In this work we compare the isotopic signatures of methane from burning in these particular regions and discuss the extent to which the regional variability of the isotopic composition of fire emissions should be taken into account in global models using isotopes to constrain the global methane budget.</p>


1999 ◽  
Vol 13 (2) ◽  
pp. 445-461 ◽  
Author(s):  
Paul Quay ◽  
John Stutsman ◽  
David Wilbur ◽  
Amy Snover ◽  
Ed Dlugokencky ◽  
...  

1999 ◽  
Vol 104 (D11) ◽  
pp. 13895-13910 ◽  
Author(s):  
Stanley C. Tyler ◽  
Henry O. Ajie ◽  
Mohan L. Gupta ◽  
Ralph J. Cicerone ◽  
Donald R. Blake ◽  
...  

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