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Buoyancy-driven destabilization of an immersed granular bed

Published online by Cambridge University Press:  26 March 2018

Eric Herbert
Affiliation:
DyCo Team, Laboratoire Interdisciplinaire des Energies de Demain, Université Paris Diderot, CNRS, 75013 Paris, France
Cyprien Morize
Affiliation:
Laboratoire FAST, CNRS, Université Paris-Sud, Université Paris-Saclay, 91405, Orsay, France
Aurélie Louis-Napoléon
Affiliation:
Institut de Mécanique des Fluides de Toulouse, IMFT, Université de Toulouse, CNRS, 31400 Toulouse, France
Christophe Goupil
Affiliation:
DyCo Team, Laboratoire Interdisciplinaire des Energies de Demain, Université Paris Diderot, CNRS, 75013 Paris, France
Pierre Jop
Affiliation:
Surface du verre et Interfaces, CNRS/Saint-Gobain, 93300 Aubervilliers, France
Yves D’Angelo*
Affiliation:
DyCo Team, Laboratoire Interdisciplinaire des Energies de Demain, Université Paris Diderot, CNRS, 75013 Paris, France Université Côte d’Azur, Laboratory Mathematics & Interactions LJAD, UNS/CNRS, 06108 Nice, France
*
Email address for correspondence: ydangelo@unice.fr

Abstract

Under suitable conditions, an immersed granular bed can be destabilized by local thermal forcing and the induced buoyant force. The destabilization is evident from the triggering and establishment of a dense fluid-like granular plume. Varying the initial granular layer average height $h$, a time series of the free layer surface is extracted, allowing us to dynamically compute the underlying volume of the granular layer. Different observed phenomena, namely the initial interface deformation, the lowering of the average granular interface (i.e. decrease of the granular layer volume) and the emission of a plume, are analysed. We show that the phenomenon is mainly driven by heat transfer, for large $h$ and also involves a variable height thermal boundary condition and Darcy flow triggering, for small $h$. Simple modelling with no adjustable parameters not only allows us to capture the observed scaling power laws but is also in quantitative agreement with the obtained experimental data.

Type
JFM Papers
Copyright
© 2018 Cambridge University Press 

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Herbert et al. supplementary movie

A typical long-run (total) evolution of the thermal destabilization and grain particles re-suspension of the granular layer, for an initial length h = 23 mm and $\Delta$ = 45 K, showing the different stages of the process. Note that the movie time is accelerated: 1 s in the movie corresponds to 12.5 s in physical time.

Download Herbert et al. supplementary movie(Video)
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