2003
DOI: 10.1016/s1359-6462(03)00446-9
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Influence of permeability on the grain refinement induced by forced convection in copper-base alloys

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Cited by 31 publications
(17 citation statements)
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“…Dedicated careful experimental studies in the microgravity environment of space are needed, in order to further clarify the mechanism of fragmentation by suppressing the effects of buoyancy. Conversely, fragmentation induced by convection in the mushy zone should be characterized during directional solidification on earth (Flemings, 2000;Beckermann, 2002;Campanella et al, 2003). Furthermore, it should be pointed out that fragmentation is a microscale phenomenon whereas the interaction of interdendritic flow with dissolution and remelting process has to be considered in a complete global model.…”
Section: Conclusion and Discussionmentioning
confidence: 99%
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“…Dedicated careful experimental studies in the microgravity environment of space are needed, in order to further clarify the mechanism of fragmentation by suppressing the effects of buoyancy. Conversely, fragmentation induced by convection in the mushy zone should be characterized during directional solidification on earth (Flemings, 2000;Beckermann, 2002;Campanella et al, 2003). Furthermore, it should be pointed out that fragmentation is a microscale phenomenon whereas the interaction of interdendritic flow with dissolution and remelting process has to be considered in a complete global model.…”
Section: Conclusion and Discussionmentioning
confidence: 99%
“…An important deduction of LSRE is that solute-rich melt will cause local dissolution (or remelting) of dendrites, when flow velocity is in the direction of increasing temperature and larger than isotherm velocity, in the reference frame of the crucible (Beckermann, 2002). When dendrite fragments formed by this local dissolution mechanism are carried into the bulk melt, they could promote columnar to equiaxed transition (CET) where local undercooling condition is favorable (Hellawell et al, 1997;Campanella et al, 2003;Spittle, 2006 A classical approach of solidification modelling is to treat the liquid and mushy regions in separate domains. The fluid motion in the melt region is modelled in general by the Navier-Stokes equations, while that within the mushy is modelled as in a porous medium (Darcy's law).…”
Section: Introductionmentioning
confidence: 99%
“…Also, the interaction between the induced current and the applied magnetic field produces EM forces, which drive the flow in the melt. The flow behavior in EM stirred melts is generally controlled by the applied magnetic field used, namely stationary, 2,7,8) rotating, 9) or traveling magnetic fields. 5,10) Moreover, the resulting flow field is highly sensitive to variations in coil design, namely the coil configuration 11,12) and the location of the coil with respect to the melt.…”
Section: Introductionmentioning
confidence: 99%
“…There are essentially two types of flow models for the mushy region, namely single-zone 7,21,22) and dual-zone models. 23,24) The single-zone model treats the entire twophase region as a porous medium, with the flow being damped via Darcy's law.…”
Section: Introductionmentioning
confidence: 99%
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