2010
DOI: 10.1007/s00231-010-0591-9
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Numerical solution of a steady natural convection flow from a vertical plate with the combined effects of streamwise temperature and species concentration variations

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Cited by 18 publications
(13 citation statements)
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“…Throughout the calculations, the conditions are used for a micropolar fl uid with Δ = 1 (corresponds to the case where the micropolar vortex viscosity is identical to the fl uid dynamic viscosity), i.e., is strongly non-Newtonian (unless otherwise indicated), with the Prandtl number Pr = 1.0 corresponding to an electrolyte solution such as salt water, and also with Sc = 0.6 that represents a diffusion chemical species of most common interest in water, for the case n = 0 (strong concentration of microelements) and B = 0.1. The value of the corresponding buoyancy force parameter (ratio of the buoyancy force due to mass diffusion to the buoyancy force due to the thermal diffusion) w takes the value 0.5 for low concentration at a = 0.5 [the effects of these parameters were mentioned earlier, see (Roy and Hossain, 2010;Chamkha et al, 2013]. The present model is reduced to a purely micropolar fl ow without porous medium effects when Da → ∞, i.e., the medium permeability becomes infi nite, so that in the limit that the Darcian drag becomes vanishingly small.…”
Section: Resultsmentioning
confidence: 99%
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“…Throughout the calculations, the conditions are used for a micropolar fl uid with Δ = 1 (corresponds to the case where the micropolar vortex viscosity is identical to the fl uid dynamic viscosity), i.e., is strongly non-Newtonian (unless otherwise indicated), with the Prandtl number Pr = 1.0 corresponding to an electrolyte solution such as salt water, and also with Sc = 0.6 that represents a diffusion chemical species of most common interest in water, for the case n = 0 (strong concentration of microelements) and B = 0.1. The value of the corresponding buoyancy force parameter (ratio of the buoyancy force due to mass diffusion to the buoyancy force due to the thermal diffusion) w takes the value 0.5 for low concentration at a = 0.5 [the effects of these parameters were mentioned earlier, see (Roy and Hossain, 2010;Chamkha et al, 2013]. The present model is reduced to a purely micropolar fl ow without porous medium effects when Da → ∞, i.e., the medium permeability becomes infi nite, so that in the limit that the Darcian drag becomes vanishingly small.…”
Section: Resultsmentioning
confidence: 99%
“…In addition, the fl uid is considered to be a gray, absorbing-emitting radiative but nonscattering medium, and the Rosseland approximation is used to describe the radiative heat fl ux in the energy equation. By invoking all of the boundary layer, Boussinesq and Rosseland diffusion approximations, the governing equations for this problem can be written as [see, for instance, (Roy and Hossain, 2010;Chamkha et al, 2013]…”
Section: Governing Equationsmentioning
confidence: 99%
“…Molla et al [20] investigated radiation effect for free convection laminar flow along a vertical flat plate with streamwise sinusoidal surface temperature. Roy and Hossain [21] studied the steady natural convection flow over a vertical flat plat with the combined effects of streamwise temperature and species concentration variation. They studied the variation of the surface shear stress coefficient with the coefficients of the rates of heat transfer.…”
Section: Introductionmentioning
confidence: 99%
“…To define the periodic array of heaters behind or within the wall, Rees [26] proposed another form of surface temperature variation with sinusoidal variations about the mean temperature which is held above the ambient temperature of the fluid. These types of boundary heating have been investigated by, among others, Pop and Ingham [27], Roy and Hossain [28], Saha et al [29], Molla et al [30], and Rana and Bhargava [31]. The momentum, heat, and mass transfer equations are reduced into nonlinear partial differential equations form.…”
Section: Introductionmentioning
confidence: 99%