Transport in Porous Media, Vol.78, No.2, 259-276, 2009
Natural Convection in a Cavity Filled with Porous Layers on the Top and Bottom Walls
Natural convection in a partially filled porous square cavity is numerically investigated using SIMPLEC method. The Brinkman-Forchheimer extended model was used to govern the flow in the porous medium region. At the porous-fluid interface, the flow boundary condition imposed is a shear stress jump, which includes both the viscous and inertial effects, together with a continuity of normal stress. The thermal boundary condition is continuity of temperature and heat flux. The results are presented with flow configurations and isotherms, local and average Nusselt number along the cold wall for different Darcy numbers from 10(-1) to 10(-6), porosity values from 0.2 to 0.8, Rayleigh numbers from 10(3) to 10(7), and the ratio of porous layer thickness to cavity height from 0 to 0.50. The flow pattern inside the cavity is affected with these parameters and hence the local and global heat transfer. A modified Darcy-Rayleigh number is proposed for the heat convection intensity in porous/fluid filled domains. When its value is less than unit, global heat transfer keeps unchanged. The interfacial stress jump coefficients beta(1) and beta(2) were varied from -1 to +1, and their effects on the local and average Nusselt numbers, velocity and temperature profiles in the mid-width of the cavity are investigated.
Keywords:Interfacial boundary condition;Porous square cavity;Natural convection;Porous/fluid domains;Stress jump