| Literature DB >> 25792960 |
Abstract
Adoption of the hyperbolic Cattaneo-Christov heat-flow model in place of the more usual parabolic Fourier law is shown to raise the possibility of oscillatory convection in the classic Bénard problem of a Boussinesq fluid heated from below. By comparing the critical Rayleigh numbers for stationary and oscillatory convection, Rc and RS respectively, oscillatory convection is found to represent the preferred form of instability whenever the Cattaneo number C exceeds a threshold value CT≥8/27π2≈0.03. In the case of free boundaries, analytical approaches permit direct treatment of the role played by the Prandtl number [Formula: see text], which-in contrast to the classical stationary scenario-can impact on oscillatory modes significantly owing to the non-zero frequency of convection. Numerical investigation indicates that the behaviour found analytically for free boundaries applies in a qualitatively similar fashion for fixed boundaries, while the threshold Cattaneo number CT is computed as a function of [Formula: see text] for both boundary regimes.Entities:
Keywords: Rayleigh–Bénard convection; buoyancy-driven instabilities; hyperbolic heat-flow; oscillatory convection; thermal convection
Year: 2015 PMID: 25792960 PMCID: PMC4353040 DOI: 10.1098/rspa.2014.0845
Source DB: PubMed Journal: Proc Math Phys Eng Sci ISSN: 1364-5021 Impact factor: 2.704