Surface rippling during solidification of binary polycrystalline alloy: Insights from 3-D phase-field simulations

被引:9
作者
Ankit, Kumar [1 ]
Xing, Hui [2 ]
Selzer, Michael [1 ,3 ]
Nestler, Britta [1 ,3 ]
Glicksman, Martin E. [4 ]
机构
[1] Karlsruhe Inst Technol, Inst Appl Mat, Haid & Neu Str 7, D-76131 Karlsruhe, Germany
[2] Northwestern Polytech Univ, Shaanxi Key Lab Condensed Matter Struct & Propert, Key Lab Space Appl Phys & Chem, Xian, Peoples R China
[3] Karlsruhe Univ Appl Sci, Inst Mat & Proc, Moltkestr 30, D-76133 Karlsruhe, Germany
[4] Florida Inst Technol, Coll Engn, 150 West Univ Blvd, Melbourne, FL 32901 USA
关键词
Phase-field modeling; Solidification; Morphological instabilities; Growth models; Diffusion-limited patterns; SOLID-LIQUID INTERFACE; COOPERATIVE GROWTH MODE; FE-C STEELS; GRAIN-BOUNDARY; EUTECTOID TRANSFORMATION; VOLUME DIFFUSION; DIRECTIONAL SOLIDIFICATION; EVOLUTION; SCALE; MICROSTRUCTURES;
D O I
10.1016/j.jcrysgro.2016.05.033
中图分类号
O7 [晶体学];
学科分类号
0702 ; 070205 ; 0703 ; 080501 ;
摘要
The mechanisms by which crystalline imperfections initiate breakdown of a planar front during directional solidification remain a topic of longstanding interest. Previous experimental findings show that the solid-liquid interface adjacent to a grain boundary provides a potential site where morphological instabilities initiate. However, interpretation of experimental data is difficult for complex 3-D diffusion fields that develop around grain multi-junctions and boundary ridges. We apply a phase-field approach to investigate factors that induce interfacial instabilities during directional solidification of a binary polycrystalline alloy. Using 2-D simulations, we establish the influence of solid-liquid interfacial energies on the spatial localization of initial interfacial perturbations. Based on parametric studies, we predict that grain misorientation and supersaturation in the melt provide major crystal growth factors determining solute segregation responsible for surface rippling. Subsequent breakdown of boundary ridges into periodic rows of hills, as simulated in 3-D, conform well with experiments. Finally, the significance of crystal misorientation relationships is elucidated in inducing spatial alignment of surface ripples. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:52 / 59
页数:8
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