UNSTEADY BUOYANCY-DRIVEN THERMAL CONVECTION IN A NON-DARCIAN POROUS MEDIUM VERTICAL CHANNEL WITH ASYMMETRIC HEATING/COOLING

被引:3
|
作者
Zueco, Joaquin [1 ]
Beg, O. Anwar [2 ]
Takhar, H. S. [3 ]
机构
[1] Tech Univ Cartagena, Dept Thermal Engn & Fluids, Cartagena 30202, Spain
[2] Sheffield Hallam Univ, Dept Heat Transfer & Mech Engn, Sheffield S1 1WB, S Yorkshire, England
[3] Manchester Metropolitan Univ, Dept Engn, Manchester M1 5GD, Lancs, England
关键词
unsteady thermo-convection; non-Darcian; isotropic; porous medium; electronic cooling; asymmetric heating/cooling; buoyancy; NSM; geothermal energy; nuclear energy systems; LAMINAR FREE CONVECTION; FORCED-CONVECTION; FLOW; LAYER;
D O I
10.1615/JPorMedia.v14.i1.60
中图分类号
O414.1 [热力学];
学科分类号
摘要
A mathematical model is presented for the transient free convection flow of a viscous, incompressible, Newtonian fluid in a parallel-plate channel configuration containing an isotropic, homogenous, non-Darcian porous material with asymmetric cooling/heating of the plates. The governing unsteady partial differential equations are formulated in an (X,Y) coordinate system and obtained from the Navier-Stokes model. Using a set of transformations, these equations with appropriate boundary conditions are rendered into a set of second-order, nonlinear (momentum), and linear (energy) partial differential equations in terms of single independent spatial variable y and dimensionless time tau. The unsteady coupled flow problem is solved using the network simulation method and the PSPICE algorithm database. The model finds applications in nuclear thermo-convection, cooling of electronic components, thermal power plant, ocean thermal energy conversion, etc.
引用
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页码:73 / 79
页数:7
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