Methane (CH4) is an important greenhouse gas with its mixing ratio increasing in the global atmosphere. Identifying fingerprints of CH4 emissions is critical to understanding potential impacts of various anthropogenic sources in the Greater Houston area (GHA) and extensive natural gas operations in the Barnett Shale area (BSA) of Texas. Stable carbon isotope ratios of CH4 (δ13CCH4) has been proposed to be a useful technique for differentiating individual CH4 sources. Measurements of CH4 mixing ratios and δ13CCH4 were sampled using a mobile laboratory equipped with cavity ring-down spectrometers (CRDS). Areal CH4 distributions and the background δ13CCH4 signature were obtained from filtered ambient signals; −47.0‰ (GHA) and − 48.5‰ (BSA) were calculated. The fingerprint of thirty-three anthropogenic sources in the two study areas were sampled with forty-four δ13C analyses conducted. Repeated measurements indicated the natural variation of δ13CCH4 signatures of individual CH4 sources. An unexpected massive CH4 fugitive leak was detected near the San Jacinto River Fleet site in Houston exhibiting an δ13CCH4 value around −42‰. Our results and findings demonstrate the utility of δ13CCH4for facilitating emission inventories and atmospheric modeling.
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