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- W2159934446 abstract "Dissolution of carbon dioxide (CO 2 ) injected into saline aquifers causes an unstable high-density diffusive front. Understanding how instability fingers develop has received much attention because they accelerate dissolution trapping, which favours long-term sequestration. The time for the onset of convection as the dominant transport mechanism has been traditionally studied by neglecting dispersion and treating the CO 2 –brine interface as a prescribed concentration boundary by analogy to a thermal convection problem. This work explores the effect of these simplifications. Results show that accounting for the CO 2 mass flux across the prescribed concentration boundary has little effect on the onset of convection. However, accounting for dispersion causes a reduction of up to two orders of magnitude on the onset time. This implies that CO 2 dissolution can be accelerated by activating dispersion as a transport mechanism, which can be achieved adopting a fluctuating injection regime." @default.
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- W2159934446 date "2009-10-19" @default.
- W2159934446 modified "2023-10-04" @default.
- W2159934446 title "Effect of dispersion on the onset of convection during CO<sub>2</sub> sequestration" @default.
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- W2159934446 doi "https://doi.org/10.1017/s0022112009991480" @default.
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