4.6 Article

The Tip of Dendritic Crystal in an Inclined Viscous Flow

Journal

CRYSTALS
Volume 12, Issue 11, Pages -

Publisher

MDPI
DOI: 10.3390/cryst12111590

Keywords

dendrite; inclined viscous flow; hydrodynamics

Funding

  1. Ministry of Science and Higher Education of the Russian Federation (Ural Federal University Program of Development within the Priority-2030 Program)

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In this study, we investigate the flow around the tip of a dendritic crystal using an inclined stream of viscous incompressible liquid. Our simulations demonstrate that the inclination of the stream has a significant impact on the hydrodynamic flow and shear stress, which leads to potential differences in heat and mass transfer mechanisms between the upstream and downstream sides of the growing dendritic crystal.
We study the flow around the tip of a dendritic crystal by an inclined stream of viscous incompressible liquid. The tip shape is chosen accordingly to recent theory [Phil. Trans. R. Soc. A 2020, 378, 20190243] confirmed by a number of experiments and computations [Phil. Trans. R. Soc. A 2021, 379, 20200326]. Our simulations have been carried out for a 0, 30, 60, and 90-degree flow slope to the dendrite axis. We show that the stream inclination has a significant effect on the hydrodynamic flow and shear stress. In particular, a transition from laminar to turbulent currents on the upstream side of the dendritic crystal may occur in an inclined hydrodynamic flow. This leads to the fact that the heat and mass transfer mechanisms on the upstream and downstream sides of a growing dendritic crystal may be different.

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