The role of incoming flow on crystallization of undercooled liquids with a two-phase layer

被引:14
|
作者
Alexandrov, Dmitri, V [1 ]
Toropova, Liubov, V [2 ,3 ]
机构
[1] Ural Fed Univ, Dept Theoret & Math Phys, Lab Multiscale Math Modeling, Lenin Ave 51, Ekaterinburg 620000, Russia
[2] Friedrich Schiller Univ Jena, Otto Schott Inst Materialforsch, D-07743 Jena, Germany
[3] Ural Fed Univ, Dept Theoret & Math Phys, Lab Math Modeling Phys & Chem Proc Multiphase Med, Lenin Ave 51, Ekaterinburg, Russia
基金
俄罗斯科学基金会;
关键词
MORPHOLOGICAL STABILITY; DENDRITE GROWTH; MUSHY LAYERS; SOLIDIFICATION; CONVECTION; TRANSPORT; CHIMNEYS;
D O I
10.1038/s41598-022-22786-w
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Motivated by important applications of crystallization phenomena, we consider a directional solidification process for a binary melt with a two-phase (mushy) layer in the presence of weak melt flow. We consider the steady-state solidification scenario, so that the two-phase layer filled with solid and liquid material keeps its thickness. In addition, we consider that the melt flows onto the two-phase layer slowly in the opposite direction to directional crystallization and solidifies there. A complete analytical solution to non-linear two-phase layer equations is constructed in a parametric form, where the solid phase fraction represents a decision variable. The temperature and solute concentration distributions, mushy layer permeability and average interdendritic spacing as well as solidification velocity and mushy layer thickness are analytically determined. We show that incoming melt flow plays a decisive role on mushy layer parameters and internal structures. The solid phase fraction within the two-phase layer and its thickness essentially grow while the mushy layer permeability and average interdendritic spacing decrease with increasing intensity of incoming melt flow.
引用
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页数:9
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