Convection in a horizontal fluid layer under an inclined temperature gradient for Prandtl numbers Pr > 1

被引:7
|
作者
Ortiz-Perez, A. S. [1 ]
Davalos-Orozco, L. A. [1 ]
机构
[1] Univ Nacl Autonoma Mexico, Inst Invest Mat, Dept Polimeros, Mexico City 04510, DF, Mexico
关键词
Thermal convection; Inclined temperature gradient; Pattern formation; Hadley circulation; Atmospheric flows; THERMAL-CONVECTION; SHALLOW CAVITY; STABILITY; DRIVEN; OSCILLATIONS;
D O I
10.1016/j.ijheatmasstransfer.2013.09.065
中图分类号
O414.1 [热力学];
学科分类号
摘要
In this paper calculations are done of the flow instability of a shallow horizontal fluid layer under an inclined temperature gradient for Prandtl numbers of magnitudes Pr > 1. In a previous paper (Ortiz-Perez and Davalos-Orozco, 2011 [17]), the range of values investigated were Pr <= 1. There, the magnitudes of the horizontal Rayleigh number investigated were far larger than those used in the literature and it was found the new oblique oscillatory mode Obo. In the present paper it is found that this oblique oscillatory mode still appears for Pr = 2. Further, it is also shown that some modes become irrelevant when the Prandtl number is increased, and different modes become the first to go unstable. An important result is that above a large enough Prandtl number, the curves of criticality remain almost the same. Therefore, the limit Pr -> infinity is employed to calculate useful analytical expressions for the longitudinal modes of criticality which cover almost all the range of horizontal Rayleigh numbers. In contrast to the authors previous results, in this paper it is shown that for Pr > 1 the transversal oscillatory mode has a range, in the horizontal Rayleigh number, as the first unstable one which first increases and then decreases with Pr, but never disappears. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:444 / 455
页数:12
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