HIGHLIGHTS
SUMMARY
In the presence of a density stratification, a layer of fluid exhibits a rich phenomenology determined by the action of gravity that can lead to oscillations and wave propagation. A typical case is represented by a single component fluid heated from below, where the stratification is determined by the thermal dilation of the fluid, which can transfer heat either in a conductive or in a convective regime. The case of a suspension of thermophilic particles heated from below is particularly interesting, because in this case the stabilizing flux of nanoparticles induced by thermophoresis competes . . .
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