Linear Rayleigh-Benard stability of a transversely isotropic fluid

被引:3
|
作者
Holloway, C. R. [1 ]
Smith, D. J. [1 ,2 ]
Dyson, R. J. [1 ]
机构
[1] Univ Birmingham, Sch Math, Birmingham B15 2TT, W Midlands, England
[2] Univ Birmingham, Inst Metab & Syst Res, Birmingham B15 2TT, W Midlands, England
基金
英国工程与自然科学研究理事会;
关键词
76E06; 76A05; 76D99; FLOW; DICHROISM; ORIENTATION; SUSPENSION; MODEL; LAYER;
D O I
10.1017/S0956792518000359
中图分类号
O29 [应用数学];
学科分类号
070104 ;
摘要
Suspended fibres significantly alter fluid rheology, as exhibited in for example solutions of DNA, RNA and synthetic biological nanofibres. It is of interest to determine how this altered rheology affects flow stability. Motivated by the fact thermal gradients may occur in biomolecular analytic devices, and recent stability results, we examine the problem of Rayleigh-Benard convection of the transversely isotropic fluid of Ericksen. A transversely isotropic fluid treats these suspensions as a continuum with an evolving preferred direction, through a modified stress tensor incorporating four viscosity-like parameters. We consider the linear stability of a stationary, passive, transversely isotropic fluid contained between two parallel boundaries, with the lower boundary at a higher temperature than the upper. To determine the marginal stability curves the Chebyshev collocation method is applied, and we consider a range of initially uniform preferred directions, from horizontal to vertical, and three orders of magnitude in the viscosity-like anisotropic parameters. Determining the critical wave and Rayleigh numbers, we find that transversely isotropic effects delay the onset of instability; this effect is felt most strongly through the incorporation of the anisotropic shear viscosity, although the anisotropic extensional viscosity also contributes. Our analysis confirms the importance of anisotropic rheology in the setting of convection.
引用
收藏
页码:659 / 681
页数:23
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