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dc.contributor.authorYaseri, Ahmed Zarzor Hussien
dc.contributor.supervisorProf. Stefan Iglaueren_US

Rock became more CO2 wet with increasing pressure, temperature and brine salinities and less CO2 wet with increasing surface roughness - i.e. a lower storage capacity can be inferred for structural trapping. Moreover, we demonstrate that gas densities correlate remarkably well with wettability also a physical model was developed to provide a theoretical framework. Furthermore, the permeability of sandstone samples reduced after injection of brine, CO2-saturated brine or supercritical CO2 at reservoir conditions.

dc.publisherCurtin Universityen_US
dc.titleCO2 wettability of rock and implications for core-floodingen_US
curtin.departmentPetroleum Engineeringen_US
curtin.accessStatusOpen accessen_US
curtin.facultyScience and Engineeringen_US

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