2001
DOI: 10.1016/s1365-1609(01)00004-1
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A salt cavern abandonment test

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Cited by 70 publications
(47 citation statements)
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“…For example, experiments performed in an airintake shaft at the WIPP site provide permeabilities as low as K = 10 -21 m 2 for undisturbed salt (Dale and Hurtado, 1997). Durup (1994) More recently, at the Etrez site, an 18-month test in a fullsized cavern provided K = 2 · 10 -19 m 2 (Bérest et al, 2001c). This larger figure is consistent with the generally accepted effects of scale on rock permeability (Brace, 1980).…”
Section: Rock Salt Permeabilitymentioning
confidence: 55%
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“…For example, experiments performed in an airintake shaft at the WIPP site provide permeabilities as low as K = 10 -21 m 2 for undisturbed salt (Dale and Hurtado, 1997). Durup (1994) More recently, at the Etrez site, an 18-month test in a fullsized cavern provided K = 2 · 10 -19 m 2 (Bérest et al, 2001c). This larger figure is consistent with the generally accepted effects of scale on rock permeability (Brace, 1980).…”
Section: Rock Salt Permeabilitymentioning
confidence: 55%
“…This in situ test, performed in a cavern at the Gaz de France storage site in Etrez, has been supported by the SMRI (Bérest et al, 2001c). Ez53 is a relatively small cavern (V = 7500 ± 500 m 3 ) leached out in Spring 1982.…”
Section: The Etrez 53 Testmentioning
confidence: 57%
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“…This is for instance the case for salt cavern abandonment where the salt creep and the brine thermal expansion can lead to pressure build-up after cavern abandonment (see e.g. Bérest et al, 2001).…”
Section: Introduction and Methodologymentioning
confidence: 99%