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• W2040337519 abstract "Convective mixing in porous media is triggered by a Rayleigh–Benard-type hydrodynamic instability as a result of an unstable density stratification of fluids. While convective mixing has been studied extensively, the fundamental behavior of the dissolution flux and its dependence on the system parameters are not yet well understood. Here, we show that the dissolution flux and the rate of fluid mixing are determined by the mean 10" @default.
• W2040337519 created "2016-06-24" @default.
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• W2040337519 date "2012-12-01" @default.
• W2040337519 modified "2023-09-24" @default.
• W2040337519 title "Scaling of Convective Mixing in Porous Media" @default.
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• W2040337519 hasPublicationYear "2012" @default.
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