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- W2041567011 abstract "Abstract The storage of carbon dioxide in deep brine‐filled permeable rocks is an important tool for CO 2 emissions mitigation on industrial scales. Residual trapping of CO 2 through capillary forces within the pore space of the reservoir is one of the most significant mechanisms for storage security and is also a factor determining the ultimate extent of CO 2 migration within the reservoir. In this study we have evaluated the impact of reservoir conditions of pressure, temperature, and brine salinity on the residual trapping characteristic curve of a fired Berea sandstone rock. The observations demonstrate that the initial‐residual characteristic trapping curve is invariant across a wide range of pressure, temperature, and brine salinities and is also the same for CO 2 ‐brine systems as a N 2 ‐water system. The observations were made using a reservoir condition core‐flooding laboratory that included high‐precision pumps, temperature control, the ability to recirculate fluids for weeks at a time, and an X‐ray CT scanner. Experimental conditions covered pressures of 5–20 MPa, temperatures of 25–50°C, and 0–5 mol/kg NaCl brine salinity. A novel coreflooding approach was developed, making use of the capillary end effect to create a large range in initial CO 2 saturation (0.15–0.6) in a single coreflood. Upon subsequent flooding with CO 2 ‐equilibriated brine, the observation of residual saturation corresponded to the wide range of initial saturations before flooding resulting in a rapid construction of the initial‐residual curve. For each condition we report the initial‐residual curve and the resulting parameterization of the Land hysteresis models." @default.
- W2041567011 created "2016-06-24" @default.
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- W2041567011 date "2015-04-01" @default.
- W2041567011 modified "2023-10-16" @default.
- W2041567011 title "The impact of reservoir conditions on the residual trapping of carbon dioxide in <scp>B</scp> erea sandstone" @default.
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- W2041567011 doi "https://doi.org/10.1002/2014wr016441" @default.
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