Dendritic growth with the six-fold symmetry: Theoretical predictions and experimental verification

被引:55
作者
Alexandrov, D. V. [1 ]
Galenko, P. K. [2 ]
机构
[1] Ural Fed Univ, Dept Theoret & Math Phys, Lab Multiscale Math Modeling, Ekaterinburg 620000, Russia
[2] Friedrich Schiller Univ Jena, Phys Astron Fak, D-07743 Jena, Germany
基金
俄罗斯科学基金会;
关键词
Growth models; Dendrites; Convection; Solvability theory; FORCED-CONVECTION; UNDERCOOLED MELTS; PATTERN-FORMATION; CRYSTAL-GROWTH; ICE CRYSTALS; MUSHY LAYER; FLOW; SOLIDIFICATION; SELECTION; ALLOYS;
D O I
10.1016/j.jpcs.2017.04.016
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
A free dendrite growing in a pure substance is considered with the interfacial effect of anisotropy and convective flow. A stable mode of dendritic growth with the six-fold crystal symmetry is studied using the solvability theory. We demonstrate that the obtained selection criterion for a stable mode of dendritic growth is a function of surface energy stiffness, arbitrary values of Peclet numbers and convective flow intensity. To predict the dendrite tip velocity V and its tip radius R a model of dendrite growth with the six-fold symmetry is formulated. We show that the model equations can be reduced to the growth kinetics with the low Peclet numbers, which exhibit the explicit relationships "tip velocity - undercooling". The model predictions are compared with experimental data on ice dendrites grown from pure undercooled water on board of the International Space Station (under microgravitational conditions, mu g) and on the Ground (under terrestrial conditions, 1 g).
引用
收藏
页码:98 / 103
页数:6
相关论文
共 55 条
[1]   Selection criterion of a stable dendrite growth in rapid solidification [J].
Alexandrov, D. V. ;
Danilov, D. A. ;
Galenko, P. K. .
INTERNATIONAL JOURNAL OF HEAT AND MASS TRANSFER, 2016, 101 :789-799
[2]   Mathematical Modeling of a Mushy Layer at the Inner Core Boundary of the Earth. Part 2. Theoretical Description [J].
Alexandrov, D. V. ;
Malygin, A. P. ;
Alexandrova, I. V. .
PROCEEDINGS OF THE INTERNATIONAL CONFERENCE OF NUMERICAL ANALYSIS AND APPLIED MATHEMATICS 2014 (ICNAAM-2014), 2015, 1648
[3]   Mathematical Modeling of a Mushy Layer at the Inner Core Boundary of the Earth. Part 1. Analytical Solutions [J].
Alexandrov, D. V. ;
Malygin, A. P. ;
Alexandrova, I. V. .
PROCEEDINGS OF THE INTERNATIONAL CONFERENCE OF NUMERICAL ANALYSIS AND APPLIED MATHEMATICS 2014 (ICNAAM-2014), 2015, 1648
[4]   Dendrite growth under forced convection: analysis methods and experimental tests [J].
Alexandrov, D. V. ;
Galenko, P. K. .
PHYSICS-USPEKHI, 2014, 57 (08) :771-786
[5]   Selection criterion for the growing dendritic tip at the inner core boundary [J].
Alexandrov, D. V. ;
Galenko, P. K. .
JOURNAL OF PHYSICS A-MATHEMATICAL AND THEORETICAL, 2013, 46 (19)
[6]   Unidirectional solidification of binary melts from a cooled boundary: analytical solutions of a nonlinear diffusion-limited problem [J].
Alexandrov, D. V. ;
Nizovtseva, I. G. ;
Malygin, A. P. ;
Huang, H-N ;
Lee, D. .
JOURNAL OF PHYSICS-CONDENSED MATTER, 2008, 20 (11)
[7]   Thermo-solutal and kinetic regimes of an anisotropic dendrite growing under forced convective flow [J].
Alexandrov, Dmitri V. ;
Galenko, Peter K. .
PHYSICAL CHEMISTRY CHEMICAL PHYSICS, 2015, 17 (29) :19149-19161
[8]   Selection criterion of stable dendritic growth at arbitrary Peclet numbers with convection [J].
Alexandrov, Dmitri V. ;
Galenko, Peter K. .
PHYSICAL REVIEW E, 2013, 87 (06)
[9]   Mushy Layer Formation during Solidification of Binary Alloys from a Cooled Wall: the Role of Boundary Conditions [J].
Alexandrova, I. V. ;
Alexandrov, D. V. ;
Aseev, D. L. ;
Bulitcheva, S. V. .
ACTA PHYSICA POLONICA A, 2009, 115 (04) :791-794
[10]   DENDRITIC GROWTH OF AN ELLIPTICAL PARABOLOID WITH FORCED-CONVECTION IN THE MELT [J].
ANANTH, R ;
GILL, WN .
JOURNAL OF FLUID MECHANICS, 1989, 208 :575-593