Journal
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Volume 16, Issue 9, Pages 2858-2864Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2015GC005936
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Funding
- Center for Frontiers of Subsurface Energy Security (CFSES) at University of Texas at Austin, an Energy Frontier Research Center - U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences [DE-SC0001114]
- National Science Foundation [EAR-0948842, EAR-1258878]
- Geology Foundation of University of Texas
- ExxonMobil
- Directorate For Geosciences
- Division Of Earth Sciences [1258878] Funding Source: National Science Foundation
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We present a new method for measuring wettability or contact angle of minerals at reservoir pressure-temperature conditions using high-resolution X-ray computed tomography (HRXCT) and radiography. In this method, a capillary or a narrow slot is constructed from a mineral or a rock sample of interest wherein two fluids are allowed to form an interface that is imaged using X-rays. After some validation measurements at room pressure-temperature conditions, we illustrate this method by measuring the contact angle of CO2-brine on quartz, muscovite, shale, borosilicate glass, polytetrafluoroethylene (PTFE or Teflon), and polyether ether ketone (PEEK) surfaces at 60-71 degrees C and 13.8-22.8 MPa. At reservoir conditions, PTFE and PEEK surfaces were found to be CO2-wet with contact angles of 140 degrees and 127 degrees, respectively. Quartz and muscovite were found to be water-wet with contact angles of 26 degrees and 58 degrees, respectively, under similar conditions. Borosilicate glass-air-brine at room conditions showed strong water-wet characteristics with a contact angle of 9 degrees, whereas borosilicate glass-CO2-brine at 13.8 MPa and 60 degrees C showed a decrease in its water-wetness with contact angle of 54 degrees. This method provides a new application for X-ray imaging and an alternative to other methods.
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