2016
DOI: 10.1016/j.jct.2015.07.031
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Receding and advancing (CO 2 + brine + quartz) contact angles as a function of pressure, temperature, surface roughness, salt type and salinity

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Cited by 193 publications
(211 citation statements)
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References 45 publications
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“…[3][4][5][6][7][8] Among all these types of CO 2 storage sites, deep saline aquifers are considered more suitable, because they have the largest CO 2 storage capacity and the widest geographical spread. 13,27,[29][30][31][32][33][34][35][36][37][38][39] Wettability, as has been previously shown in laboratory experiments (at the mm to cm scale), has a significant effect on residual trapping 15,[40][41][42] and structural trapping. Indeed, water contact angles between 0°(strongly water-wet) and 170°(strongly CO 2 -wet) have been measured, where CO 2 -wettability mainly depends on the surface chemistry, and to a lesser extent on temperature, pressure, and brine composition.…”
Section: Introductionmentioning
confidence: 54%
“…[3][4][5][6][7][8] Among all these types of CO 2 storage sites, deep saline aquifers are considered more suitable, because they have the largest CO 2 storage capacity and the widest geographical spread. 13,27,[29][30][31][32][33][34][35][36][37][38][39] Wettability, as has been previously shown in laboratory experiments (at the mm to cm scale), has a significant effect on residual trapping 15,[40][41][42] and structural trapping. Indeed, water contact angles between 0°(strongly water-wet) and 170°(strongly CO 2 -wet) have been measured, where CO 2 -wettability mainly depends on the surface chemistry, and to a lesser extent on temperature, pressure, and brine composition.…”
Section: Introductionmentioning
confidence: 54%
“…reported that increasing water salinity from 0 wt% (DI water) to 20 wt% leads to an increase in advancing contact angle by 16° (from 59 o to 75 o ) and an increase in receding contact angle by 12° (from 54 o to 66 o ) for a mica surface at 323 K and 15 MPa. Similarly, significant increases were measured for quartz . This effect is caused by a better surface charge screening at higher salinities.…”
Section: Introductionmentioning
confidence: 57%
“…This increase in migration distance with increasing salinity is caused by the shift in the characteristics curves (i.e. relative permeability and capillary pressure); recall that salinity affects the CO 2 ‐rock wettability, and increasing brine salinity leads to reduced water wettability …”
Section: Resultsmentioning
confidence: 99%
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“…Al-Anssari et al [129] investigated the influence of pressure on the wettability of calcites treated with and without nanoparticles in the presence of CO 2 to account for pressure variation with injection depth. An increase in pressure with increase in contact angle occurred for all surfaces tested which is attributed to an increase in intermolecular interactions between CO 2 and calcite, which increased significantly with increasing CO 2 density thus an implication of a reduction in structural and residual trapping capacities at reservoir conditions [126][127][128][130][131][132][133]. At ambient condition, oil-wet calcite was weakly CO 2 -wet (115 θa -0.1 MPa and 323 K) and strongly CO 2 -wet at storage conditions (148 θa -20 MPa and 323 K) -the high contact angle is an indication of possibilities of CO 2 leakage.…”
Section: Co 2 Storage and Leakage Inhibitionmentioning
confidence: 91%