2014
DOI: 10.1007/s11661-014-2252-y
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A Phase-Field Model for the Diffusive Melting of Isolated Dendritic Fragments

Abstract: A thermal phase-field model constructed in the 'thin-interface' limit and incorporating a number of advanced numerical techniques as such adaptive mesh refinement, implicit time-stepping and a multigrid solver has been used to study the isolated diffusive melting of dendritic fragments. The results of the simulations are found to be fully consistent with the experimental observation of such melting in microgravity during the Isothermal Dendrite Growth Experiment. It is found that the rate at which the ratio of… Show more

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Cited by 2 publications
(1 citation statement)
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“…During terrestrial melting, by contrast, where gravity is present, buoyancy convection and rapid sedimentation totally obscure the onset of shape changes. Several aspects of these experimental observations in microgravity were later reproduced in a phase-field simulation of melting crystallites reported by Mullis [15]. Mullis's numerical results provided the first inkling that conventional phase-field simulations, without modification, might also produce interface fields responsible for transformation-induced shape changes.…”
Section: Experimental Observations: Capillaryinduced Shape Changementioning
confidence: 84%
“…During terrestrial melting, by contrast, where gravity is present, buoyancy convection and rapid sedimentation totally obscure the onset of shape changes. Several aspects of these experimental observations in microgravity were later reproduced in a phase-field simulation of melting crystallites reported by Mullis [15]. Mullis's numerical results provided the first inkling that conventional phase-field simulations, without modification, might also produce interface fields responsible for transformation-induced shape changes.…”
Section: Experimental Observations: Capillaryinduced Shape Changementioning
confidence: 84%