Abstract

This study presents a meteorologically-based methodology for quantifying basin-scale methane (CH4) emissions in Utah’s Uintah Basin, which is home to over 9,000 active and producing oil and natural gas wells. Previous studies in oil and gas producing regions have often relied on intensive aircraft campaigns to estimate methane emissions. However, the high cost of airborne campaigns prevents their frequent undertaking, thus providing only daytime snapshots of emissions rather than more temporally-representative estimates over multiple days. Providing estimates of CH4 emissions from oil and natural gas production regions across the United States is important to inform leakage rates and emission mitigation efforts in order to curb the potential impacts of these emissions on global climate change and local air quality assessments. Here we introduce the Basin-constrained Emissions Estimate (BEE) method, which utilizes the confining topography of a basin and known depth of a pollution layer during multi-day wintertime cold-air pool episodes to relate point observations of CH4 to basin-scale CH4 emission rates. This study utilizes ground-based CH4 observations from three fixed sites to calculate daily increases in CH4, a laser ceilometer to estimate pollution layer depth, and a Lagrangian transport model to assess the spatial representativity of surface observations. BEE was applied to two cold-air pool episodes during the winter of 2015–2016 and yielded CH4 emission estimates between 44.60 +/– 9.66 × 103 and 61.82 +/– 19.76 × 103 kg CH4 hr–1, which are similar to the estimates proposed by previous studies performed in the Uintah Basin. The techniques used in this study could potentially be utilized in other deep basins worldwide.

Highlights

  • Global methane (CH4) levels have increased over the past several decades, with numerous studies attributing the rise at least partially to increased anthropogenic emissions (Bruhwiler et al 2017; Miller et al 2013; Nisbet et al 2016; Saunois et al 2016, 2017; Sheng et al 2018; Thompson et al 2018; Turner et al 2016, 2017, 2019)

  • Basin-constrained Emissions Estimate (BEE) was applied to two cold-air pool episodes during the winter of 2015–2016 and yielded CH4 emission estimates between 44.60 +/– 9.66 × 103 and 61.82 +/– 19.76 × 103 kg CH4 hr–1, which are similar to the estimates proposed by previous studies performed in the Uintah Basin

  • HPL and Castle Peak (CSP) observed generally higher estimated daily increases in observed CH4 compared to ROO, which is consistent with expectations of higher local emissions due to the higher density of oil and natural gas (ONG) industry in the vicinity of HPL and CSP

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Summary

Fasoli The University of Utah

Follow this and additional works at: https://digitalcommons.usu.edu/bingham SeePnaerxttopfatghee fEonrvairdodnimtioennatal al Mutohnoirtsoring Commons, and the Oil, Gas, and Energy Commons. C.S., Crosman, E.T., Horel, J.D., Lyman, S., Fasoli, B., Bares, R. and Lin, J.C., 2019. Quantifying methane emissions in the Uintah Basin during wintertime stagnation episodes. This study presents a meteorologically-based methodology for quantifying basin-scale methane (CH4) ­emissions in Utah’s Uintah Basin, which is home to over 9,000 active and producing oil and natural gas wells. Previous studies in oil and gas producing regions have often relied on intensive aircraft c­ampaigns to e­stimate methane emissions. BEE was applied to two cold-air pool episodes during the winter of 2015–2016 and yielded CH4 emission estimates between 44.60 +/– 9.66 × 103 and 61.82 +/– 19.76 × 103 kg CH4 hr–1, which are similar to the estimates proposed by previous studies performed in the Uintah Basin. The t­echniques used in this study could potentially be utilized in other deep basins worldwide

Introduction
Data and Methods
Results and Discussion

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