During CO
2 storage, CO
2 plume mixes with the water and oil present at the reservoir, initiated by diffusion followed by a density gradient that leads to a convective flow. Studies are available where CO
2 convective mixing have been studied in
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During CO
2 storage, CO
2 plume mixes with the water and oil present at the reservoir, initiated by diffusion followed by a density gradient that leads to a convective flow. Studies are available where CO
2 convective mixing have been studied in water phase but limited in oil phase. This study was conducted to reach this gap, and experiments were conducted in a vertically packed 3-dimensional column with oil-saturated unconsolidated porous media at 100 bar and 50 °C (representative of reservoir pressure and temperature conditions).
N-Decane and crude oil were used as oils, and glass beads as porous media. A bromothymol blue water solution-filled sapphire cell connected at the bottom of the column was used to monitor the CO
2 breakthrough. With the increase of the Rayleigh number, the CO
2 transport rate in
n-decane was found to increase as a function of a second order polynomial.
number vs. dimensionless time
had a power relationship in the form of
. The overall pressure decay was faster in
n-decane compared to crude oil for similar permeability (4 D), and the crude oil had a breakthrough time three times slower than in
n-decane. The results were compared with similar experiments that have been carried out using water.
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