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Fluxes of methane, non-methane hydrocarbons and carbon dioxide from natural gas well pad soils in Eastern Utah
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  • Seth Lyman, Utah State University

We measured fluxes of methane, non-methane hydrocarbons, and carbon dioxide from natural gas well pad soils and from nearby undisturbed soils in eastern Utah. Methane fluxes varied from less than zero to more than 38,000 mg m-2 h-1. Fluxes from well pad soils were almost always greater than from undisturbed soils. Fluxes were greater from locations with higher concentrations of total combustible gas in soil and were inversely correlated with distance from well heads. Several lines of evidence show that the majority of emission fluxes (about 70%) were due to subsurface sources of raw gas that migrated to the atmosphere, with the remainder likely caused by re-emission of spilled liquid hydrocarbons. Total hydrocarbon fluxes in summer were only 27% as high as during winter, likely because soil bacteria consumed the majority of hydrocarbons during summer months, converting them to carbon dioxide. While this study shows that well pad soils are a meaningful hydrocarbon emission source at some wells, well pad soil emissions are not significant relative to the oil and gas industry overall. We estimate that well pad soils account for much less than 1% of total emissions of methane and non-methane hydrocarbons from the oil and gas industry in Utah's Uinta Basin.

Document Type
File Format
Publication Date
Utah State University
Funding Agency

US Dept. of Interior, Bureau of Land Management

U.S. Department of Energy, contract number 12122-15

Research Partnership to Secure Energy for America

Award Number
BLM Cooperative Agreement number L13AC00292 and U.S. Department of Energy; contract number 12122-15

see associated publication for collection and processing of data.

Eastern Utah
Code Lists

See the ReadMe file for descriptions of parameters and variables.

Creative Commons Public Domain Mark 1.0
Citation Information
Seth Lyman. "Fluxes of methane, non-methane hydrocarbons and carbon dioxide from natural gas well pad soils in Eastern Utah" (2017)
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