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Flooding of coastal areas with seawater often leads to density stratification. The stability of the density-depth profile in a porous medium initially saturated with a fluid of density $$\rho _\mathrm{f}$$ ρ f after flooding with a salt solution of higher density $$\rho _\mathrm{s}$$ ρ s is analyzed. The standard convection/diffusion equation subject to the so-called Boussinesq approximation...
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