Heat transfer of thermocapillary convection in a two-layered fluid system under the influence of magnetic field

被引:8
作者
Cha, Soyoung S. [1 ]
Ramachandran, Narayanan [2 ]
Worek, William M. [1 ]
机构
[1] Univ Illinois, Chicago, IL 60607 USA
[2] NASA, George C Marshall Space Flight Ctr, Jacobs ESTS Grp, Huntsville, AL 35812 USA
关键词
IMMISCIBLE LIQUID LAYERS; MARANGONI CONVECTION; NATURAL-CONVECTION; FREE-SURFACE; BUOYANCY; FLOW;
D O I
10.1016/j.actaastro.2009.01.018
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
Heat transfer of a two-layer fluid system has been of great importance in a variety of industrial applications. For example, the phenomena of immiscible fluids can be found in materials processing and heat exchangers. Typically in solidification from a melt, the convective motion is the dominant factor that affects the uniformity of material properties. In the layered flow, thermocapillary forces can come into an important play, which was first emphasized by a previous investigator in 1958. Under extraterrestrial environments without gravity, thermocapillary effects can be a more dominant factor, which alters material properties in processing. Control and optimization of heat transfer in an immiscible fluid system need complete understanding of the flow phenomena that can be induced by surface tension at a fluid interface. The present work is focused on understanding of the magnetic field effects on thermocapillary convection, in order to optimize material processing. That is, it involves the study of the complicated phenomena to alter the flow motion in crystal growth. In this effort, the Marangoni convection in a cavity with differentially heated sidewalls is investigated with and without the influence of a magnetic field. As a first step, numerical analyzes are performed, by thoroughly investigating influences of all pertinent physical parameters. Experiments are then conducted, with preliminary results, for comparison with the numerical analyzes. (C) 2009 Elsevier Ltd. All fights reserved.
引用
收藏
页码:1066 / 1079
页数:14
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