Convective instability of directional crystallization in a forced flow: the role of brine channels in a mushy layer on nonlinear dynamics of binary systems

DOI10.1016/j.ijheatmasstransfer.2010.11.008zbMath1225.80005OpenAlexW2089423140MaRDI QIDQ631152

A. P. Malygin, Dmitri V. Alexandrov

Publication date: 22 March 2011

Published in: International Journal of Heat and Mass Transfer (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/j.ijheatmasstransfer.2010.11.008

zbMATH Keywords

crystallizationbrine channelsmushy layersea icessolid-liquid phase transitions

Mathematics Subject Classification ID

Stefan problems, phase changes, etc. (80A22) Turbulent transport, mixing (76F25) Forced convection (76R05)

Related Items (7)

Nucleation and growth of ellipsoidal crystals in a supercooled binary melt ⋮ Thermo-solutal and kinetic modes of stable dendritic growth with different symmetries of crystalline anisotropy in the presence of convection ⋮ Analytical solution of integro‐differential equations describing the process of intense boiling of a superheated liquid ⋮ On the theory of the unsteady-state growth of spherical crystals in metastable liquids ⋮ Effects of nonlinear growth rates of spherical crystals and their withdrawal rate from a crystallizer on the particle-size distribution function ⋮ On the theory of crystal growth in metastable systems with biomedical applications: protein and insulin crystallization ⋮ Convective boundary integral equation: the case of a non-axisymmetric dendrite with a forced viscous flow

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