Entropy Generation at Natural Convection in an Inclined Rectangular Cavity

被引:38
作者
Bouabid, Mounir [1 ]
Magherbi, Mourad [2 ]
Hidouri, Nejib [1 ]
Ben Brahim, Ammar [1 ]
机构
[1] Gabes Univ, Engn Natl Sch Gabes, Dept Chem & Proc Engn, Gabes 6029, Tunisia
[2] Gabes Univ, High Inst Appl Sci & Technol, Dept Civil Engn, Gabes 6029, Tunisia
来源
ENTROPY | 2011年 / 13卷 / 05期
关键词
natural convection; rectangular cavity; entropy generation; numerical methods; IN TRIANGULAR PRISM; FORCED-CONVECTION; PLANE CHANNEL; DUCT; FLOW;
D O I
10.3390/e13051020
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
Natural convection in an inclined rectangular cavity filled with air is numerically investigated. The cavity is heated and cooled along the active walls whereas the two other walls of the cavity are adiabatic. Entropy generation due to heat transfer and fluid friction has been determined in transient state for laminar natural convection by solving numerically: the continuity, momentum and energy equations, using a Control Volume Finite Element Method. The structure of the studied flows depends on four dimensionless parameters which are: the thermal Grashof number, the inclination angle, the irreversibility distribution ratio and the aspect ratio of the cavity. The obtained results show that entropy generation tends towards asymptotic values for lower thermal Grashof number values, whereas it takes an oscillative behavior for higher values of thermal Grashof number. Transient entropy generation increases towards a maximum value, then decreases asymptotically to a constant value that depends on aspect ratio of the enclosure. Entropy generation increases with the increase of thermal Grashof number, irreversibility distribution ratio and aspect ratio of the cavity. Bejan number is used to measure the predominance of either thermal or viscous irreversibility. At local level, irreversibility charts show that entropy generation is mainly localized on bottom corner of the left heated wall and upper corner of the right cooled wall.
引用
收藏
页码:1020 / 1033
页数:14
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