An entropy generation analysis of horizontal convection under the centrifugal buoyancy approximation. (April 2022)

• Record Type: Journal Article
• Authors: Mayeli, Peyman; Sheard, Gregory J.
• Is Part Of: International communications in heat and mass transfer. Volume 133(2022)
• Publication Date: 2022-04
• Subjects: Horizontal convection -- Centrifugal buoyancy approximation -- Gay-Lussac parameter -- Entropy generation analysis; Heat -- Transmission -- Periodicals; Mass transfer -- Periodicals; Chaleur -- Transmission -- Périodiques; Transfert de masse -- Périodiques; Heat -- Transmission; Mass transfer; Periodicals; 621.4022
• DOI: 10.1016/j.icheatmasstransfer.2022.105923
• Languages: English
• ISSNs: 0735-1933

Abstract

Abstract: An entropy generation analysis is conducted for horizontal convection under the centrifugal buoyancy and the Boussinesq approximations in a relatively shallow enclosure at a fixed Prandtl number of unity to characterise irreversible losses across the conduction and convection-dominated regimes using the Bejan number ( Be ). A variable irreversibility distribution factor is expressed for the entropy generation analysis as a ratio of the Brinkman number ( Br ) and the Gay-Lussac ( Ga ) parameter for the first time. Governing equations are solved numerically using a high-order nodal spectral-element method. Calculations are performed at a fixed Br = 2 × 10 −5 over the physical range of the Gay-Lussac parameter 0 ≤ Ga ≤ 2 up to Ra = 5 × 10 8 . As expected, increasing the Rayleigh number shifts the flow toward a convection-dominated regime; however it is found that increasing the Gay-Lussac parameter draws the heat transfer mechanism back to a conduction-dominated state. In other words, advection related buoyancy effects act to keep the buoyancy-driven flow in conduction-dominated regime. The entropy generation analysis indicates that at Ga ≳ 0.5 conduction and convection are in balance at Ra ≈ 6 × 10 5, while under the conventional Boussinesq approximation ( Ga = 0), heat transfer is convection-dominated. The transition of the average Bejan number from conduction to convection-dominated regime follows closely to a reciprocal scaling against Rayleigh number Be ave ~ Ra −1 when Ga = 0 but the same process scales with Be ave ~ Ra −0.5 relation at Ga = 2.