2012
DOI: 10.1007/s11242-012-0096-8
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Viscous Dissipation and Thermal Radiation Effects on Mixed Convection from a Vertical Plate in a Non-Darcy Porous Medium

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Cited by 9 publications
(14 citation statements)
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References 25 publications
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“…Utilizing the Oberbeck‐Boussinesq approximation, continuity, momentum, and nanoparticle concentration equations can be written as (Kairi and Murthy, Narayana et al, and Murthy et al) x(rmu)goodbreakinfix+y(rmv)goodbreakinfix=0, uy+cKnormalpμ/ρfu2y=(1C)gρfKpβcosγμTy(ρnormalpρnormalf)gKpcosγμCy, uTx+vTy=α2Ty2+τ[DnormalB(Ty)2+DTTtrue(TyCytrue)]+μρfKCpu(u+ρnormalfcKμu2)1ρcpqry, …”
Section: Problem Formulationmentioning
confidence: 99%
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“…Utilizing the Oberbeck‐Boussinesq approximation, continuity, momentum, and nanoparticle concentration equations can be written as (Kairi and Murthy, Narayana et al, and Murthy et al) x(rmu)goodbreakinfix+y(rmv)goodbreakinfix=0, uy+cKnormalpμ/ρfu2y=(1C)gρfKpβcosγμTy(ρnormalpρnormalf)gKpcosγμCy, uTx+vTy=α2Ty2+τ[DnormalB(Ty)2+DTTtrue(TyCytrue)]+μρfKCpu(u+ρnormalfcKμu2)1ρcpqry, …”
Section: Problem Formulationmentioning
confidence: 99%
“…The respective temperature and nanoparticle concentrations in the ambient medium are defined as ∞ T and ∞ C , respectively. Utilizing the Oberbeck-Boussinesq approximation, continuity, momentum, and nanoparticle concentration equations can be written as (Kairi and Murthy, 5 Narayana et al, 25 and Murthy et al 36 ) where components of the velocity along x-and y-directions are defined as u and v, respectively. The empirical constant (c) is a function of Forchheimer porous inertia term, K p is the permeability, μ ρ and f are defined as the viscosity and density of the nanofluid, respectively, g is the acceleration due to gravity, ∞ C is the ambient concentration of the nanoparticle, γ is the half angle of the cone with the vertical axis, β is defined by the volumetric thermal expansion coefficient of the nanofluid, τ ε ρc ρc = ( ) /( ) p f , D B and D T are the Brownian diffusion coefficient and the thermophoresis diffusion coefficient, respectively, C p is the specific heat at constant pressure, and ∞ T is the ambient temperature.…”
Section: Problem Formulationmentioning
confidence: 99%
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“…Indeed, it has been emphasized by Rees and Magyari and Nield that a mixed or forced‐convection boundary‐layer flow generates heat everywhere when the viscous dissipation is present, including the free stream region outside the boundary layer. For an exhaustive discussion of the mixed convective flow due to a vertical plate immersed in a non‐Darcy porous medium saturated with a Newtonian fluid in the presence of viscous dissipation, the reader is referred to the works of Narayana and colleagues (also see the references cited therein).…”
Section: Introductionmentioning
confidence: 99%
“…Comparison of Dimensionless Similarity Functions θ′(η) for Mixed Convection Along a Vertical Flat Plate in Non-Darcy Porous Medium with Nb → 0, Nt = Nr = 0, ε = 0.1, χ 2 = 1, Re * = 1, and S(η) → 0 (Narayana and colleagues[17]) Effects of modified Reynolds number Re * on (a) velocity, (b) temperature, and (c) volume fraction profiles.…”
mentioning
confidence: 99%