Turbulent natural convection in a porous square cavity computed with a macroscopic κ-ε model

被引:60
作者
Braga, EJ [1 ]
de Lemos, MJS [1 ]
机构
[1] ITA, Dept Energy, IEME, BR-12228900 Sao Jose Dos Campos, Brazil
基金
巴西圣保罗研究基金会;
关键词
turbulence modeling; porous media; heat transfer; natural convection;
D O I
10.1016/j.ijheatmasstransfer.2004.07.017
中图分类号
O414.1 [热力学];
学科分类号
摘要
Detailed numerical computations for faminar and turbulent natural convection within a square cavity filled with a fluid saturated porous medium are presented. Heated vertical walls are maintained at constant but different temperatures, while horizontal surfaces are kept insulated. The macroscopic kappa-epsilon turbulence model with wall function is used to handle turbulent flows in porous media. In this work, the turbulence model is first switched off and the laminar branch of the solution is found when increasing the Rayleigh number, Ra-m. Computations covered the range 10 < Ra-m < 10(6) and 10(-7) < Da < 10(-10) and made use of the finite volume method. Subsequently, the turbulence model is included and calculations start at high Ra-m, merging to the laminar branch for a reducing Ra-m and for Ra-m less than a certain critical Rayleigh number, Ra-cr. This convergence of results as Ra-m decreases can be seen as a characterization of the laminarization phenomenon. For Ra-m values less than around 10(4), both laminar and turbulent flow solutions merge, indicating that such critical value for Ra-m was reached. Results further indicate that when the parameters porosity, Pr, conductivity ratio between the fluid and the solid matrix and the Ra-m are kept fixed, the lower the Darcy number, the higher the average Nusselt number at the hot wall. (C) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:5639 / 5650
页数:12
相关论文
共 48 条
[1]
A general two-equation macroscopic turbulence model for incompressible flow in porous media [J].
Antohe, BV ;
Lage, JL .
INTERNATIONAL JOURNAL OF HEAT AND MASS TRANSFER, 1997, 40 (13) :3013-3024
[2]
NATURAL-CONVECTION FLOW IN A SQUARE CAVITY REVISITED - LAMINAR AND TURBULENT MODELS WITH WALL FUNCTIONS [J].
BARAKOS, G ;
MITSOULIS, E ;
ASSIMACOPOULOS, D .
INTERNATIONAL JOURNAL FOR NUMERICAL METHODS IN FLUIDS, 1994, 18 (07) :695-719
[3]
Free convection in oblique enclosures filled with a porous medium [J].
Baytas, AC ;
Pop, I .
INTERNATIONAL JOURNAL OF HEAT AND MASS TRANSFER, 1999, 42 (06) :1047-1057
[4]
Bear J., 1988, DYNAMICS FLUIDS PORO
[5]
BECKERMANN C, 1986, NUMER HEAT TRANSFER, V10, P557, DOI 10.1080/10407788608913535
[6]
BOUNDARY-LAYER REGIME IN A VERTICAL ENCLOSURE FILLED WITH A POROUS-MEDIUM [J].
BEJAN, A .
LETTERS IN HEAT AND MASS TRANSFER, 1979, 6 (02) :93-102
[7]
Benard H, 1901, ANN CHIM PHYS, V23, P62
[8]
DAVIS GD, 1983, INT J NUMER METH FL, V3, P249
[9]
Modeling of double-diffusive turbulent natural convection in porous media [J].
de Lemos, MJS ;
Tofaneli, LA .
INTERNATIONAL JOURNAL OF HEAT AND MASS TRANSFER, 2004, 47 (19-20) :4233-4241
[10]
Turbulent mass transport in saturated rigid porous media [J].
de Lemos, MJS ;
Mesquita, MS .
INTERNATIONAL COMMUNICATIONS IN HEAT AND MASS TRANSFER, 2003, 30 (01) :105-113