2008
DOI: 10.1016/j.asr.2007.06.038
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Comparative study of the influence of natural convection on directional solidification of Al–3.5wt% Ni and Al–7wt% Si alloys

Abstract: We present numerical simulations of thermosolutal convection for directional solidification of Al-3.5 wt% Ni and Al-7 wt% Si. Numerical results predict that fragmentation of dendrite arms resulting from dissolution could be favored in Al-7 wt% Si, but not in Al-3.5 wt% Ni. Corresponding experiments are in qualitative agreement with the numerical predictions. Distinguishing the two fragmentation mechanisms, namely dissolution and remelting, is critical during experiments on earth, when fluid flow is dominant.

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Cited by 18 publications
(12 citation statements)
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“…Then, natural convection in general changes the thermal and solutal conditions ahead of the dendrite front and also in the mushy zone [3,9]. Based on previous results [15,19,26,50], from both experiments and simulations, the qualitative liquid flow patterns induced by the gravity in the mushy zone and ahead of the dendrite front during the solidification can be estimated in this experiment. In practice, solutal convection dominates in the case of metallic alloys owing to their large Lewis number defined as the ratio of the thermal diffusivity to the solutal one (Le = D th /D), typically of the order of 10 3 to 10 4 .…”
Section: The Natural Convection Flow and Its Effect On Cetmentioning
confidence: 97%
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“…Then, natural convection in general changes the thermal and solutal conditions ahead of the dendrite front and also in the mushy zone [3,9]. Based on previous results [15,19,26,50], from both experiments and simulations, the qualitative liquid flow patterns induced by the gravity in the mushy zone and ahead of the dendrite front during the solidification can be estimated in this experiment. In practice, solutal convection dominates in the case of metallic alloys owing to their large Lewis number defined as the ratio of the thermal diffusivity to the solutal one (Le = D th /D), typically of the order of 10 3 to 10 4 .…”
Section: The Natural Convection Flow and Its Effect On Cetmentioning
confidence: 97%
“…Generally speaking, in presence of gravity and depending on the alloy (partition coefficient k and respective densities of alloy elements), the convection flow is different in the two regions illustrated in Fig.8 [15,26,50]: within the mushy layer (generally considered as a porous medium) and in the region ahead of the mush/liquid interface. In the latter case, the characteristic length scale may vary from several times the solutal length D/V (V being the solidification velocity) up to the sample size far from the S/L interface.…”
Section: The Natural Convection Flow and Its Effect On Cetmentioning
confidence: 99%
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“…One alternative is to include the different physical levels (micro-, meso-and macroscopic) or the two-level (micro-macro) strategy, but with the inconvenience of requiring large computational resources. A second alternative uses macroscopic models that include the macroscopic influence on the system properties and behavior [1][2][3][4][5][6][7].…”
Section: Introductionmentioning
confidence: 99%