2016
DOI: 10.18280/ijht.34s245
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Transient Natural Convection in Partially Porous Vertical Annuli

Abstract: The numerical modeling of natural convection in partially porous annuli is a topic of rising interest, due to its practical applications for the provisional analyses of several engineering applications such as geothermal down-hole heat exchangers, chemical reactors, etc. Though a large number of papers focused on the modeling of this phenomenon under steady-state conditions, only few works consider its transient thermal evolution and no works are available referred to partially porous annular cavities. However… Show more

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Cited by 26 publications
(16 citation statements)
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“…Laminar, incompressible AH flow and heat transfer in the eye are described using the GPM model. [33][34][35][36][37] The flow and temperature fields are calculated taking into account buoyancy effects, incorporated using the Boussinesq approximation, relating density differences to temperature differences in the cornea, lens, and iris, obtaining a mixed convection regime. 38,39 The equations of the GPM model are reported in the following:…”
Section: Governing Equationsmentioning
confidence: 99%
“…Laminar, incompressible AH flow and heat transfer in the eye are described using the GPM model. [33][34][35][36][37] The flow and temperature fields are calculated taking into account buoyancy effects, incorporated using the Boussinesq approximation, relating density differences to temperature differences in the cornea, lens, and iris, obtaining a mixed convection regime. 38,39 The equations of the GPM model are reported in the following:…”
Section: Governing Equationsmentioning
confidence: 99%
“…Moreover, heat transport between solid and fluid phases is considered to be negligible. The heat transport in the subsurface is described as [64,65] ρc p eq ∂T ∂t…”
Section: Governing Equationsmentioning
confidence: 99%
“…where μ is the viscous coefficient of the fluid, Pa·s; α is the permeability, m 2 ; C is the inertial resistance coefficient, m − 1 ; |υ|is the speed, m/s. e permeability α and inertial resistance coefficient C can be calculated according to the Blake-Kozeny equation [48][49][50]:…”
Section: Momentum Equation Of Porous Mediamentioning
confidence: 99%