9.1 Compositional Comparison of Volatile Organic Compounds (VOCs) from Oil and Natural Gas Activities in 13 Major U.S. Shale Basins

Tuesday, 24 January 2017: 4:00 PM
401 (Washington State Convention Center )
Jessica B. Gilman, NOAA, Boulder, CO; and B. M. Lerner, T. Tokarek, A. Koss, B. Yuan, J. Peischl, T. B. Ryerson, C. Warneke, and J. de Gouw

Compositional comparison of volatile organic compounds (VOCs) from oil and natural gas activities in 13 major U.S. shale basins

J.B. Gilman, J.B. [1], B.M. Lerner [1,2], T. Tokarek [3], A. Koss [1,2], B. Yuan [1,2], C. Warneke [1,2], J. Peischl [1,2], T.B. Ryerson [1], and J.A. de Gouw [1]

[1] NOAA Chemical Sciences Division, Boulder, CO, 80305

[2] Cooperative Institute for Research in Environmental Sciences, Boulder, CO, 80305

[3] Department of Chemistry, University of Calgary, Calgary, AB, Canada

Abstract:

The recent and unprecedented increase in oil and natural gas production from shale formations is associated with a rise in the production of methane (CH4) and non-methane volatile organic compounds (VOCs) including natural gas plant liquids (e.g., ethane, propane, and butanes) and liquid lease condensate (e.g., pentanes, hexanes, aromatics and cycloalkanes).  Since 2010, the production of natural gas liquids and the amount of natural gas vented/flared has increased by factors of approximately 1.3 and 1.6, respectively [U.S. Energy and Information Administration], indicating an increasingly large potential source of hydrocarbons to the atmosphere. 

Here we present measurements of a full suite of carbon-containing gases emitted from oil and gas activities in 13 U.S. shale basins in order to better understand their potential air quality impacts.  These measurements were made between 2011-2015 aboard the NOAA WP-3D research aircraft or at various ground sites.  Aircraft measurements of non-methane hydrocarbons were measured using a whole air sampler (WAS) with post-flight analysis via gas chromatography-mass spectrometry (GC-MS).  The discrete whole air samples are complimented by near-continuous measurements of methane (Picarro spectrometer), ethane (Aerodyne spectrometer), and VOCs (H3O+ chemical ionization mass spectrometer).  We will (i) compare the composition of methane and VOC emissions for each basin in order to show that each shale basin has a unique VOC source signature, and (ii) quantify emission fluxes of VOCs for a subset of these basins.

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