2015
DOI: 10.1021/es503882b
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Stream Measurements Locate Thermogenic Methane Fluxes in Groundwater Discharge in an Area of Shale-Gas Development

Abstract: The environmental impacts of shale-gas development on water resources, including methane migration to shallow groundwater, have been difficult to assess. Monitoring around gas wells is generally limited to domestic water-supply wells, which often are not situated along predominant groundwater flow paths. A new concept is tested here: combining stream hydrocarbon and noble-gas measurements with reach mass-balance modeling to estimate thermogenic methane concentrations and fluxes in groundwater discharging to st… Show more

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Cited by 45 publications
(83 citation statements)
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References 30 publications
(89 reference statements)
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“…Typically, once the pressure of a free-phase gas is dissipated, geysering and bubbling subside or even cease, which allows for re-entrainment of water and suppression of further gas release (Gorody 2012). These plumes of dissolved natural gases migrate advectively and can persist in shallow aquifers until they are mitigated by aerobic oxidation, biodegradation, or discharge to the surface (Van Stempvoort et al 2005;Etiope et al 2009;Molofsky et al 2013;Jackson et al 2013aJackson et al , 2013bDarrah et al 2014Darrah et al , 2015aHeilweil et al 2015Heilweil et al , 2016Wen et al 2016). These plumes of dissolved natural gases migrate advectively and can persist in shallow aquifers until they are mitigated by aerobic oxidation, biodegradation, or discharge to the surface (Van Stempvoort et al 2005;Etiope et al 2009;Molofsky et al 2013;Jackson et al 2013aJackson et al , 2013bDarrah et al 2014Darrah et al , 2015aHeilweil et al 2015Heilweil et al , 2016Wen et al 2016).…”
Section: Occurrence Of Stray Gas Migration and Factors That Control Gmentioning
confidence: 99%
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“…Typically, once the pressure of a free-phase gas is dissipated, geysering and bubbling subside or even cease, which allows for re-entrainment of water and suppression of further gas release (Gorody 2012). These plumes of dissolved natural gases migrate advectively and can persist in shallow aquifers until they are mitigated by aerobic oxidation, biodegradation, or discharge to the surface (Van Stempvoort et al 2005;Etiope et al 2009;Molofsky et al 2013;Jackson et al 2013aJackson et al , 2013bDarrah et al 2014Darrah et al , 2015aHeilweil et al 2015Heilweil et al , 2016Wen et al 2016). These plumes of dissolved natural gases migrate advectively and can persist in shallow aquifers until they are mitigated by aerobic oxidation, biodegradation, or discharge to the surface (Van Stempvoort et al 2005;Etiope et al 2009;Molofsky et al 2013;Jackson et al 2013aJackson et al , 2013bDarrah et al 2014Darrah et al , 2015aHeilweil et al 2015Heilweil et al , 2016Wen et al 2016).…”
Section: Occurrence Of Stray Gas Migration and Factors That Control Gmentioning
confidence: 99%
“…Nonetheless, in the absence of chemical or biological degradation, this methane would only be transported to other areas in the subsurface or discharge to the atmosphere through springs or hyporheic interactions (Heilweil et al 2015(Heilweil et al , 2016Kang et al 2016). The complexity arises from the dynamic interplay among buoyancy, capillary, and dispersive forces, as well as chemical and biological reactions, which are together hard to fully capture in numerical simulations.…”
Section: How Long Do Dissolved and Free Gaseous Methane Persist?mentioning
confidence: 99%
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“…There is concern regarding the potential impacts of gas and fluid movement, as well as depressurisation, on groundwater quality and quantity in adjacent aquifers used to support other industries (Atkins et al, 2015;Heilweil et al, 2015;Iverach et al, 2015;Moritz et al, 2015;Owen et al, 2016;Zhang and Soeder, 2016).…”
Section: Introductionmentioning
confidence: 99%