B038-0017
The importance of utilizing multiple methane source tracers when measuring European cities.

Wednesday, 9 December 2020
Poster
Julianne Fernandez1, James L France2, Malika Menoud3, Marius Paul Corbu4, Rebecca Fisher2, David Lowry2, Thomas Röckmann5 and Euan G Nisbet2, (1)Royal Holloway University of London, Department of Earth Sciences, Egham, TW20, United Kingdom, (2)Royal Holloway, University of London, Egham, United Kingdom, (3)Institute for Marine and Atmospheric Research Utrecht, Utrecht, Netherlands, (4)INCAS - National Institute for Aerospace Research "Elie Carafoli", Research and Development Department, Bucharest, Romania, (5)Utrecht University, Utrecht, Netherlands
Abstract:
Recent research, dominated by studies in the United States, has shown that CH4 emissions from urban areas depend on the design, age, and maintenance record of the natural gas distribution networks (NGDN). Compared to U.S cities, European cities are typically older, denser, utilize different hydrocarbon reservoirs for heating and transport, and have a wide range of cultural and behavioral styles, all of which affect emission patterns. Municipal policies are dictated by local social and economic priorities, with widely variable maintenance practices for the underlying infrastructure such as gas and sewage pipelines. These practices impact the extent of CH4 emissions and the degree of mixing of source types.

Here, we compare δ13C, δ2H, and C2:C1 source signatures between an Eastern European city (Bucharest, Romania) and a Western European city (London, U.K). Stable isotopes (δ13C-CH4) and ethane:methane (C2:C1) ratios can be used to verify whether emissions are associated with leaks from the NGDN. During extensive mobile surveys conducted between 2018 and 2019, to evaluate CH4 emissions, air samples were collected and analyzed using continuous flow gas chromatograph isotope ratio mass spectrometers for δ13C at Royal Holloway, University of London and δ2H at Utrecht University, The Netherlands. An LGR Ultraportable CH4/C2H6 Analyzer and a Picarro G4302 were used for C2:C1 ratios.

The NGDN in Bucharest had a δ13C of -49‰, δ2H of -175‰, and 0.02 for C2:C1; and London had a δ13C of -40‰, δ2H of -130‰, and 0.02 to 0.06 for C2:C1. Bucharest δ13C signatures for CH4 enhancements ranged from -64 to -36‰ and showed a normal population distribution, reflecting a dominance of mixed sources. However, δ2H ranged from -388 to -157‰ and has a bimodal distribution, indicating a clear contribution of 2 source types. For London, δ13C sources ranged from -60 to -35‰ and are positively skewed, highlighting the dominance of gas leak sources over the few waste sources. For Bucharest, the δ2H signature is a more significant tracer since δ13C of gas is isotopically light, and because gas & sewage source signatures overlap. Measurements of N2O, NH3, & H2S, can also be used for separation of sewage emissions. As Europe seeks to cut urban emissions, multiple source tracers will help identify causes of emissions from street level sources.