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Shaping of melting and dissolving solids under natural convection

Published online by Cambridge University Press:  13 August 2020

Samuel S. Pegler Open the ORCID record for Samuel S. Pegler [Opens in a new window]  and
Megan S. Davies Wykes Open the ORCID record for Megan S. Davies Wykes [Opens in a new window]
Samuel S. Pegler*
Affiliation:
School of Mathematics, University of Leeds, LeedsLS2 9JT, UK
Megan S. Davies Wykes
Affiliation:
Department of Engineering, University of Cambridge, CambridgeCB2 1PZ, UK
*
†Email address for correspondence: sam.s.pegler@gmail.com
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Abstract

How quickly does an ice cube melt or a lump of sugar dissolve? We address the open problem of the shapes of solids left to melt or dissolve in an ambient fluid driven by stable natural convection. The theory forms a convective form of a Stefan problem in which the evolution is controlled by a two-way coupling between the shape of the body and stable convection along its surface. We develop a new model describing the evolution of such bodies in two-dimensional or axisymmetric geometries and analyse it using a combination of numerical and analytical methods. Different initial conditions are found to lead to different fundamental shapes and descent rates. For the cases of initially linear surfaces (wedges or cones), the model admits similarity solutions in which the tip descends from its initial position as $t^{4/5}$, where t is time. It is determined that the evolving shape always forms a parabola sufficiently near the tip. For steeply inclined bodies, we establish a general two-tiered asymptotic structure comprising a broad $4/3$-power intermediate near-tip region connected to a deeper parabolic region at the finest scale. The model results apply universally for any given relationship between density, viscosity, diffusivity and concentration, including two-component convection. New laboratory experiments involving the dissolution of cones of sugar candy in water are found to collapse systematically onto our theoretically predicted shapes and descent rates with no adjustable parameters.

JFM classification

Phase change: Solidification/melting Convection: Buoyant boundary layers

Information

Type
JFM Papers
Information
Journal of Fluid Mechanics , Volume 900 , 10 October 2020 , A35
Copyright
© The Author(s), 2020. Published by Cambridge University Press

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References

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Pegler and Davies Wykes supplementary movie 1

Real-time shadow graph of our experiment, illustrating the transition from laminar to turbulent flow.
Download Pegler and Davies Wykes supplementary movie 1(Video)
Video 6 MB

Pegler and Davies Wykes supplementary movie 2

The evolution of experiment A.
Download Pegler and Davies Wykes supplementary movie 2(Video)
Video 5.8 MB

Pegler and Davies Wykes supplementary movie 3

The evolution of experiment B.
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Video 2.9 MB

Pegler and Davies Wykes supplementary movie 4

The evolution of experiment C.
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Video 2.9 MB

Pegler and Davies Wykes supplementary movie 5

The evolution of experiment D.
Download Pegler and Davies Wykes supplementary movie 5(Video)
Video 2 MB