2005
DOI: 10.2172/966666
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Potential for Natural Gas Storage in Deep Basalt Formations at Canoe Ridge, Washington State: A Hydrogeologic Assessment

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Cited by 6 publications
(5 citation statements)
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“…The Miocene basalts and associated shallow sedimentary interbeds have been mapped and studied for almost a century in this region, primarily in relation to aquifer usage, nuclear repository work at the Hanford Site, and more recently in regard to hydrocarbon exploration (Bretz, 1917;Montgomery, 2008;Reidel et al, 2005;Spane et al, 2003;Waters, 1961). The basalt sequestration target examined in this study is the thick (>2000 m) stack of Grande Ronde porous and permeable basalt flow tops that occur below the massive and laterally extensive Umtanum flow Tolan et al, 1989).…”
Section: Geological Settingmentioning
confidence: 99%
“…The Miocene basalts and associated shallow sedimentary interbeds have been mapped and studied for almost a century in this region, primarily in relation to aquifer usage, nuclear repository work at the Hanford Site, and more recently in regard to hydrocarbon exploration (Bretz, 1917;Montgomery, 2008;Reidel et al, 2005;Spane et al, 2003;Waters, 1961). The basalt sequestration target examined in this study is the thick (>2000 m) stack of Grande Ronde porous and permeable basalt flow tops that occur below the massive and laterally extensive Umtanum flow Tolan et al, 1989).…”
Section: Geological Settingmentioning
confidence: 99%
“…There were two energy storage projects focused on inetrflow basalt aquifers in the Columbia Basin, using UGS, CAES and UTES technologies, which launched by the U.S. Department of Energy (DOE), the Bonneville Power Administration (BPA), the Pacific Northwest National Laboratory (PNNL) and a number of energy companies in recent years [1,2,3,4,5,6]. These three technologies of energy storage play important roles in peak-shaving, supply interruptions, production storage and so on.…”
Section: Energy Storage Projects In Columbia Basin Basalt Group (Crbg)mentioning
confidence: 99%
“…Representative basaltic flow consists of a permeable flow top, a dense-impermeable flow interior, and a flow bottom with variable thickness. Contact zone between two independent basalt flows is referred to as an interflow zone, as well as the primary aquifers in the region [1,2,3]. The location map of Columbia Basin and nearby natural gas supply lines are shown in Fig.…”
Section: Energy Storage Projects In Columbia Basin Basalt Group (Crbg)mentioning
confidence: 99%
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“…Outcrop geometries, together with petrography, geochemistry, and lateral extent relationships indicate that the CRBG continental flood basalts formed as continuous, laterally extensive sheets, rather than as compound flows with discontinuous lenticular layers (Hooper; Tolan et al, 2009). The massive interiors of more thick and laterally extensive basalt flows may form regional intraformational seals that isolate groundwater within underlying basalt flowtop horizons, and can be reflected by distinct differences in hydrologic heads and hydrochemical/isotopic differences in fluid geochemistry with depth within the basalt formation (Gephart, et al, 1979, DOE 1988, Reidel et al 2005. The low-permeability, sealing properties of massive flow interiors were demonstrated during direct field tests conducted within deep boreholes on the Hanford Site as part of the BWIP basalt characterization investigation (e.g., Gephart et al, 1979, Eslinger 1986, DOE, 1988, and locally within the Wallula Pilot Borehole (McGrail et al, 2009).…”
Section: Site Selection Overviewmentioning
confidence: 99%