International Conference and Exhibition, Melbourne, Australia 13-16 September 2015 2015
DOI: 10.1190/ice2015-2210011
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An Experimental Study on the Flood Characteristic and Fluid Rock Interactions of a Supercritical CO2, Brine, Rock System

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Cited by 3 publications
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“…A synthetic brine was prepared by dissolving 40 g of NaCl and 20 g of KCl in ultrapure deionized (DI) water. It is worth noting that in this work, to eliminate or reduce two-way mass transfer (immiscible coreflooding), the brine and scCO 2 were mutually pre-equilibrated using a stirred reactor (autoclave reactor) following a technique similar to that described by Saeedi et al 47 All of the chemicals were used as received.…”
Section: Materials Sample Preparation and Test Proceduresmentioning
confidence: 99%
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“…A synthetic brine was prepared by dissolving 40 g of NaCl and 20 g of KCl in ultrapure deionized (DI) water. It is worth noting that in this work, to eliminate or reduce two-way mass transfer (immiscible coreflooding), the brine and scCO 2 were mutually pre-equilibrated using a stirred reactor (autoclave reactor) following a technique similar to that described by Saeedi et al 47 All of the chemicals were used as received.…”
Section: Materials Sample Preparation and Test Proceduresmentioning
confidence: 99%
“…(2) The pore pressure was increased to the experimental value by injecting degassed brine, and the sample was left to age and saturate with the brine for 24 h. To eliminate two-way mass transfer during CO 2 injection and achieve immiscible displacement, five pore volumes (PV) of the brine which was pre-equilibrated with CO 2 was injected to displace the degassed brine. 22,47 (3) The absolute permeability of the rock sample was measured using a multirates (1, 2, 4 cc/min) injection procedure.…”
Section: Materials Sample Preparation and Test Proceduresmentioning
confidence: 99%
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“…Queensland (e.g. the CTSCo Surat CCS project) (Dawson et al, 2015a;Harkin et al, 2017;79 Hodgkinson and Grigorescu, 2012; Saeedi et al, 2016). The Precipice Sandstone is a low 80 salinity fresh to brackish aquifer with a predicted high prospectivity for CO2 storage (Farquhar et 81 al., 2013;Horner et al, 2014).…”
mentioning
confidence: 99%