The Bénard problem for quasi-thermal-incompressible materials: A linear analysis
In this paper we apply the ideas introduced with the so-called extended-quasi-thermal-incompressible (EQTI) model, recently proposed by Gouin and Ruggeri (Int. J. Non-Linear Mech. 47 (2012) 688–693) [12]. In particular, in the Oberbeck–Boussinesq approximation we consider the more realistic constitu...
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Veröffentlicht in: | International journal of non-linear mechanics 2014-12, Vol.67, p.178-185 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | In this paper we apply the ideas introduced with the so-called extended-quasi-thermal-incompressible (EQTI) model, recently proposed by Gouin and Ruggeri (Int. J. Non-Linear Mech. 47 (2012) 688–693) [12]. In particular, in the Oberbeck–Boussinesq approximation we consider the more realistic constitutive equation compatible with the thermodynamical stability by putting in the buoyancy term a density which depends not only by the temperature but also on the pressure. The equation for the pressure is then modified by an extra dimensionless parameter β^ which is proportional to the positive compressibility factor β. The 2-D linear instability of the thermal conduction solution in horizontal layers heated from below (Bénard problem) is investigated. It is shown that for any β^: (i) the rest state pressure profile is different from the parabolic one; (ii) if convection arises, then it first arises via a stationary state and the strong principle of exchange of stability holds; for small β^: (iii) convection certainly arises provided Ra is sufficiently large; (iv) the related critical Rayleigh number coincides -in the limit of vanishing β^ – with the classical one, and decreases as β^ increases.
•We generalize the Oberbeck–Boussinesq approximation by putting in the buoyancy term a density which depends also on the pressure.•The rest state pressure profile is different from the parabolic one.•If convection arises, then it first arises via a stationary state and the strong principle of exchange of stability holds.•Convection certainly arises provided Ra is sufficiently large.•The related critical Rayleigh number decreases as the compressible factor increases. |
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ISSN: | 0020-7462 1878-5638 |
DOI: | 10.1016/j.ijnonlinmec.2014.09.003 |