1997
DOI: 10.1016/s0017-9310(97)00008-2
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Natural convective heat transfer in a fluid saturated variable porosity medium

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Cited by 519 publications
(318 citation statements)
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“…The values for 0 ε , b and c chosen to be 0.38, 1, and 2 respectively. These values were found to give good approximation to the variable porosity data given by Nithiarasu et al [12] for a particle diameter d=5 mm. The type of decay of porosity as the normal distance increases given by Equation (4) is well established and has been used extensively in studies on flow in porous media with variable porosity.…”
Section: Mathematical Analysissupporting
confidence: 67%
See 1 more Smart Citation
“…The values for 0 ε , b and c chosen to be 0.38, 1, and 2 respectively. These values were found to give good approximation to the variable porosity data given by Nithiarasu et al [12] for a particle diameter d=5 mm. The type of decay of porosity as the normal distance increases given by Equation (4) is well established and has been used extensively in studies on flow in porous media with variable porosity.…”
Section: Mathematical Analysissupporting
confidence: 67%
“…Equations (1) through (3) are supplemented by constitutive equations for the variations of the porosity permeability and thermal conductivity of the porous medium. It has been shown by Vafai [21] that the results obtained experimentally by Nithiarasu et al [12 ] in their study on void fraction distribution in packed beds gives the functional dependence of the porosity on the normal distance from the boundary and so the porosity can be represented by the exponential form 0 (e x p ( / ) )…”
Section: Mathematical Analysismentioning
confidence: 99%
“…All the example problems for flow in porous media have been taken from Nithiarasu et al [21,22]. We then proceed to model a directional binary alloy solidification example.…”
Section: Numerical Examplesmentioning
confidence: 99%
“…This problem is obtained from [22]. The dimensionless 1 × 1 domain along with the boundary conditions for velocity and temperature are shown in Figure 5.…”
Section: Example 2: Natural Convection In a Fluid Saturated Variable mentioning
confidence: 99%
“…Recently, the Lattice Boltzmann method (LBM) has been widely used in the field relevant to fluid flow and gas transport at the mesoscale because of its efficiency and effectiveness in the implementation of multiple interparticle interactions and complex geometry boundary conditions [13][14][15]. Nithiarasu et al [16] proposed a generalized Navier-Stokes equation for isothermal incompressible flow in porous media, which ignores the detailed structure of the porous media by including an additional term to account for the presence of a porous medium. Guo and Zhao [9] developed an LB model which can be used to solve the generalized Navier-Stokes equations.…”
Section: Introductionmentioning
confidence: 99%