The accurate quantification of methane emissions from point sources is required to better quantify emissions for sector-specific reporting and inventory validation. An unmanned aerial vehicle (UAV) serves as a platform to sample plumes near to source. This paper describes a near-field Gaussian plume inversion (NGI) flux technique, adapted for downwind sampling of turbulent plumes, by fitting a plume model to measured flux density in three spatial dimensions. The method was refined and tested using sample data acquired from eight UAV flights, which measured a controlled release of methane gas. Sampling was conducted to a maximum height of 31 m (i.e. above the maximum height of the emission plumes). The method applies a flux inversion to plumes sampled near point sources. To test the method, a series of random walk sampling simulations were used to derive an NGI upper uncertainty bound by quantifying systematic flux bias due to a limited spatial sampling extent typical for short-duration small UAV flights (less than 30 min). The development of the NGI method enables its future use to quantify methane emissions for point sources, facilitating future assessments of emissions from specific source-types and source areas. This allows for atmospheric measurement-based fluxes to be derived using downwind UAV sampling for relatively rapid flux analysis, without the need for access to difficult-to-reach areas.
Abstract. Atmospheric ethane can be used as a tracer to distinguish
methane sources, both at the local and global scale. Currently, ethane can be
measured in the field using flasks or in situ analyzers. In our study, we
characterized the CRDS Picarro G2201-i instrument, originally designed to
measure isotopic CH4 and CO2, for measurements of ethane-to-methane ratio in mobile-measurement scenarios, near sources and under field
conditions. We evaluated the limitations and potential of using the CRDS
G2201-i to measure the ethane-to-methane ratio, thus extending the
instrument application to simultaneously measure two methane source proxies
in the field: carbon isotopic ratio and the ethane-to-methane ratio. First,
laboratory tests were run to characterize the instrument in stationary
conditions. Subsequently, the instrument performance was tested in field
conditions as part of a controlled release experiment. Finally, the
instrument was tested during mobile measurements focused on gas compressor
stations. The results from the field were afterwards compared with the
results obtained from instruments specifically designed for ethane
measurements. Our study shows the potential of using the CRDS G2201-i
instrument in a mobile configuration to determine the ethane-to-methane
ratio in methane plumes under measurement conditions with an ethane
uncertainty of 50 ppb. Assuming typical ethane-to-methane ratios ranging
between 0 and 0.1 ppb ppb−1, we conclude that the instrument can
accurately estimate the “true” ethane-to-methane ratio within 1σ
uncertainty when CH4 enhancements are at least 1 ppm, as can be found
in the vicinity of strongly emitting sites such as natural gas compressor
stations and roadside gas pipeline leaks.
The effect of a bilayer area on the electronic response to environmental gating of a monolayer graphene Hall bar device is investigated using room temperature magnetotransport and scanning Kelvin probe microscopy measurements in a controlled environment. The device is tuned through the charge neutrality point with n-p-n-junctions formed. Scanning Kelvin probe measurements show that the work function of the monolayer graphene decreases more than that of the bilayer area however magnetotransport measurements show a larger change in carrier concentration for bilayer graphene with environmental gating. Interface scattering at the boundary between the monolayer and bilayer regions also affects device response with field-dependent suppression of the conductivity observed near the charge neutrality point.Simultaneous electronic and environmental scanning Kelvin probe measurements are used to build nano-scale maps of the work function of the device surface revealing the areas of greatest work function change with environmental gating.
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