Destabilization of an immersed granular bed by thermal convection
Members: E. Herbert, A. Sauret and C. Morize.
The transport, dispersion and resuspension of particles
occur in industrial fluid dynamical processes as well as environmental and geophysical situations. Whereas
the resuspension of an immersed granular bed by fluid flows such as vortices or shear flows has been
the focus of many studies, the ability to fluidize particles with a vertical gradient of temperature remains
poorly understood. Using laboratory experiments with a localized heat source, we observe that a massive
entrainment of particles into the fluid volume occurs beyond a threshold temperature. The buoyancy driven
fluidized bed then leads to the transport of solid particles through the generation of particle-laden plumes.
We show that the destabilization process is driven by the thermal conductivity inside the granular bed
and demonstrate that the threshold temperature depends on the thickness of the granular bed and the buoyancy
number, i.e., the ratio of the stabilizing density contrast to the destabilizing thermal density contrast.
Publications
Buoyancy driven destabilization of an immersed granular bed
E. Herbert, C. Morize, A. Louis-Napoleon, C. Goupil, P. Jop, Y. D'Angelo, J. Fluid Mech. 843, 778-809 (2018).
[Abstract | PDF | suppl. material ]
Resuspension threshold of a granular bed by localized heating
C. Morize, E. Herbert, A. Sauret, Phys. Rev. E 66, 032903 (2017).
[Abstract | PDF]
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