Linear Rayleigh-B\'enard stability of a transversely-isotropic fluid

TL;DR

This paper investigates how transversely-isotropic fluid rheology affects Rayleigh-Bénard convection stability, revealing that anisotropic viscosities delay the onset of instability, with implications for biomolecular device flows.

Contribution

It provides the first linear stability analysis of Rayleigh-Bénard convection in transversely-isotropic fluids considering a range of anisotropic parameters.

Findings

Transversely-isotropic effects delay instability onset.

Anisotropic shear viscosity has a strong stabilizing effect.

Extensional viscosity also influences stability.

Abstract

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-B\'enard 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.