Scaling approach of the convective drying of a porous medium

We propose a simplified, theoretical approach of the evolution of liquid distribution during the convective drying of a granular packing. In the absence of gravity effects three regimes are distinguished according to the relative importance of surface evaporation, capillarity or evaporation from the interior of the sample. The evolution of the drying rate as a function of the saturation can be inferred from the characteristic velocities associated to each of these effects. We also carried out during experiments of bead packings saturated with ethanol, at four different velocities of the boundary convection current; and with bead size ranging from 4.5 to 100 mu m. The drying curves exhibit different regimes with a scaling as a function of particle radius and current velocity as predicted by the theory.