A computational study of the effects of buoyancy-driven convection on const
rained melting of phase change materials within spherical containers is pre
sented. The computations are based on an iterative, finite-volume numerical
procedure using primitive-dependent variables, whereby the time-dependent
continuity, momentum and energy equations in the spherical coordinate syste
m are solved. A single-domain enthalpy formulation is used for simulation o
f the phase change phenomenon. The effect of phase change on convection is
accounted for using a Darcy's law-type porous media treatment. Early during
the melting process, the conduction mode of heat transfer is dominant, giv
ing rise to concentric temperature contours. As the buoyancy-driven convect
ion is strengthened due to the growth of the melt zone, melting in the top
legion of the sphere is much faster than in the bottom region due to the en
hancement of the conduction mode of heat transfer. When buoyancy effects ar
e very marked, as many as three time-dependent recirculating vortices are o
bserved. In comparison to the diffusion-controlled melting, buoyancy-driven
convection accelerates the melting process markedly. The Prandtl number pl
ays an important role in the melting process. With the Rayleigh number fixe
d, changing the Prandtl number from 0.03 to 1.0 and 50 brings about totally
different flow and melting patterns. The computational findings are verifi
ed through qualitative constrained melting experiments using a high-Prandtl
number wax as the phase change material. (C) 2001 Elsevier Science Ltd. Al
l rights reserved.