Heterogeneity reduces dissolution while increasing gravity current speed proportionally to Rayleigh number, accelerates convection onset in unstable cases, and interacts with anisotropy and variance to control mixing efficiency, sometimes making homogeneous media outperform heterogeneous ones.
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Mixing and spreading of gravity currents in heterogeneous porous media
Heterogeneity reduces dissolution while increasing gravity current speed proportionally to Rayleigh number, accelerates convection onset in unstable cases, and interacts with anisotropy and variance to control mixing efficiency, sometimes making homogeneous media outperform heterogeneous ones.