2016
DOI: 10.1021/acs.est.6b03111
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Pore Scale Observations of Trapped CO2 in Mixed-Wet Carbonate Rock: Applications to Storage in Oil Fields

Abstract: Residual trapping, CO 2 Storage, mixed-wet carbonate, Enhanced Oil Recovery, micro X-ray 9 CT, carbon utilization. Geologic CO 2 storage has been identified as key to avoiding dangerous climate change. 13Storage in oil reservoirs dominates the portfolio of existing projects due to favorable 14 economics. However, in an earlier related work, Al-Menhali and Krevor (2016), it was 15 identified that an important trapping mechanism, residual trapping, is weakened in rocks with

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Cited by 64 publications
(61 citation statements)
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“…Importantly, these characteristics curves have a significant influence on CO 2 migration . Furthermore, CO 2 migration increases with decreasing S gr 16 and thus with decreasing water‐wettability (note that S gr decreases when water wettability is reduced …”
Section: Resultsmentioning
confidence: 97%
See 1 more Smart Citation
“…Importantly, these characteristics curves have a significant influence on CO 2 migration . Furthermore, CO 2 migration increases with decreasing S gr 16 and thus with decreasing water‐wettability (note that S gr decreases when water wettability is reduced …”
Section: Resultsmentioning
confidence: 97%
“…Importantly, S gr decreases with increasing brine salinity, because higher salinity increases CO 2 ‐wettability and S gr is a function of wettability (i.e. increasing CO 2 wettability reduces S gr ) . Furthermore, lower salinity (i.e., lower CO 2 ‐wettability) shifts the k rw curves downwards, and the k rw ‐k rg intercept point toward the right (i.e., to a higher residual water saturation, Fig.…”
Section: Methodsmentioning
confidence: 94%
“…In CGS, structural CO 2 trapping is the principal storage mechanism whereby shale (in its classical caprock role), if strongly water‐wet, provides an efficient seal to the reservoir disallowing upward CO 2 migration [ Arif et al ., ; Armitage et al ., ; Chaudhary et al ., ; Iglauer et al ., ]. However, rock material can be even strongly CO 2 ‐wet [ Arif et al ., ; Iglauer et al ., ; Iglauer , ]—which would massively reduce storage capacity [ Al‐Menhali et al ., ; Chaudhary et al ., ; Iglauer et al , , ]—and shale wettability has so far only been reported for low‐total organic content (TOC) shales [ Chaudhary et al ., ; Iglauer et al ., ; Roshan et al ., ; Shojai Kaveh et al ., ] despite the fact that shales can be very rich in organic carbon, i.e., high TOC [ Vernik and Milovac , ].…”
Section: Introductionmentioning
confidence: 99%
“…The qualitative observations of residual water structures in Figure are similar to Han et al () who examined the distribution of residual water structures with XCT and noted larger multipore water ganglia in mixed‐wetting systems. Similarly, Al‐Menhali et al () noted that residual CO 2 structures also favored larger, multipore ganglia in mixed‐wetting systems. Bench‐scale experimental studies of scCO 2 trapping have hypothesized the formation of large, multipore residual ganglia in IW systems (e.g., Alyafei & Blunt, ); however, this has never been confirmed.…”
Section: Resultsmentioning
confidence: 86%
“…The disruption of water films in altered wetting media reduces film straining, an important colloid retention mechanism in unsaturated systems, increasing colloid transport (Han et al, ; Wan & Tokunaga, ). Geologic reservoirs that are either IW or NW will possess lower carbon trapping efficiencies than WW reservoirs (Al‐Menhali et al, ; Al‐Menhali & Krevor, ; Alyafei & Blunt, ; Broseta et al, ; Chaudhary et al, ; Chiquet et al, ; Iglauer et al, ; Krevor et al, ; Krevor et al, ; Pentland et al, ).…”
Section: Introductionmentioning
confidence: 99%