Mathematical Problems in Engineering

Volume 2016, Article ID 4017076, 12 pages

http://dx.doi.org/10.1155/2016/4017076

## Analytical and Numerical Study on Magnetoconvection Stagnation-Point Flow in a Porous Medium with Chemical Reaction, Radiation, and Slip Effects

^{1}School of Engineering, Asia Pacific University of Technology and Innovation, 57000 Kuala Lumpur, Malaysia^{2}Institute of Mathematical Sciences, University of Malaya, 50603 Kuala Lumpur, Malaysia^{3}Department of Mechanical Engineering, University of Malaya, 50603 Kuala Lumpur, Malaysia

Received 24 December 2015; Revised 19 March 2016; Accepted 27 March 2016

Academic Editor: Vassilios C. Loukopoulos

Copyright © 2016 H. Niranjan et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

#### Abstract

We investigate the effects of slip and radiation on magnetoconvection flow of a chemically reacting fluid near a stagnation-point towards a vertical plate embedded in a porous medium analytically and numerically. The governing partial differential equations are diminished into the coupled ordinary differential equations by similarity transformations. Then they are solved analytically by homotopy analysis method and solved numerically by shooting method with RK fourth-order method. In this study, the analytical and numerical results are compared for many combinations of parameters. The rates of heat and mass transfer are calculated. The velocity profile near the plate overshoots on increasing the slip parameter. The concentration and temperature are decreasing on increasing the slip parameter.

#### 1. Introduction

The study of convective heat transfer through porous medium for an incompressible fluid on the heated surface has received major attention because of its diverse uses in the insulation of nuclear reactors, petroleum industry, geothermal problems, storage of nuclear waste, and several other areas. The study of slip condition on convective boundary layer flow beside a vertical plate embedded in a porous medium has accepted considerable practical and theoretical awareness. The research has been maintained out in this area to analyze the heat and mass transfer characteristics within the boundary layer flow. Hiemenz [1] is the pioneer to investigate the forced convection two-dimensional flow at stagnation-point by similarity transformation. Many researchers extended Crane’s [2] problem of steady flow of an incompressible fluid over a linearly stretched plate to analyze several conditions. Mohammadi [3] numerically analyzed on boundary layer natural convection flow along a vertical plate. Cheng et al. [4] developed an analytic solution by homotopy analysis method for an unsteady mixed convection flow near the stagnation-point towards a vertical surface in a porous medium. Layek et al. [5] studied the boundary layer flow near stagnation-point in a porous medium over a stretching sheet with heat generation and blowing/suction. Lee et al. [6] studied convective heat transfer over a persuaded plate in a porous medium using Lie group analysis. They perceived that the thickness of the thermal and momentum boundary layer increases on increasing the radiation parameter. The natural convection flow over a plate in a porous medium was examined by Ferdows et al. [7], Rosali et al. [8], and Hou [9]. Bhuvaneswari et al. [10] studied the internal heat generation effect on natural convective flow over an inclined surface in a porous medium. They observed that the profiles of velocity and temperature increase on increasing the heat generation parameter.

The research on magnetohydrodynamic (MHD) flow and heat transfer has several applications in engineering fields such as power generator, design of MHD accelerators, cooling of nuclear reactors, and heat exchangers. The effect of radiation on heat and mass transfer is essential in some applications, such as hydrometallurgical industries, solar power technology, and astrophysical flows. Takhar et al. [11] and Aydin and Kaya [12] explored the mixed magnetoconvection of a viscous fluid in the surrounding area of a stagnation-point next to a heated vertical surface. Hayat et al. [13] considered the mixed convection stagnation-point flow towards a sheet in a porous medium with magnetic field and radiation effects using homotopy analysis method. Makinde [14] studied the effects of internal heat generation and radiation on MHD mixed convection stagnation-point flow in a perpendicular plate embedded in a porous medium.

The study of chemical reaction on heat and mass transfer is very significant in chemical technology and food processing. Bhuvaneswari et al. [15] studied the effect of chemical reaction on a semi-infinite inclined surface using Lie group analysis. Bhattacharyya [16] and Afify and Elgazery [17] investigated the two-dimensional flow of a viscous fluid with chemical reaction over a stretching/shrinking sheet near a stagnation-point. Recently, boundary layer flow with slip condition has attracted many researchers. Abel and Mahesha [18] analyzed the characteristics of MHD flow of a non-Newtonian viscoelastic fluid over a stretching sheet in the presence of nonuniform radiation and heat source. Hari et al. [19] numerically analyzed the effect of chemical reaction on MHD mixed convective flow over a vertical plate embedded in a porous medium with thermal radiation. The velocity and concentration increase on increasing the values of the chemical reaction parameter in the case of generative case and they are decreasing in the case of destructive case. Makinde and Sibanda [20] investigated the effects of chemical reaction and internal heat generation on the boundary layer flow over a linearly stretching sheet. The local skin friction and mass transfer rate increase on increasing the Schmidt number. Bhattacharyya and Layek [21] analyzed steady, laminar stagnation-point flow in a porous shrinking sheet with radiation and suction. Wang [22] and Labropulu and Li [23] examined the effect of slip of a non-Newtonian fluid behavior at a stagnation-point flow over a plate. Harris et al. [24] and Bhattacharyya et al. [25] explored the steady mixed convection flow at a stagnation-point in a porous medium over a perpendicular surface with velocity slip condition. Merkin et al. [26] and Rohni et al. [27] considered temperature slip effect on an unsteady boundary layer flow in a porous medium. Aman et al. [28] and Seini and Makinde [29] studied the MHD flow of an incompressible fluid over a linearly shrinking/stretching sheet with slip effects. Singh and Chamkha [30] examined the heat transfer and fluid flow near the vertical linear shrinking sheet using second-order slip condition. They noticed that the skin friction falls on increasing the slip parameter. Roşca and Pop [31] explored steady forced flow and convection heat transfer over a vertical shrinking/stretching sheet using slip condition.

Inspired by the above applications and surveys explained, the purpose of this present study is to explore the effects of chemical reaction and velocity slip on mixed convection stagnation-point flow over a vertical plate embedded in a porous medium in the presence of external magnetic field and thermal radiation.

#### 2. Mathematical Model

Consider a steady, 2D laminar, mixed convection boundary layer flow of an incompressible viscous fluid near a stagnation-point along a vertical plate in the presence of magnetic field through a porous medium as exposed in Figure 1. It is presumed that the chemical reaction is considered as homogeneous and of first order. It is supposed that the porous medium is heat generating or absorbing internally at a fixed rate. Constant strength is enforced on unvarying magnetic field along the -axis. The induced magnetic field is negligible due to small magnetic Reynolds number. As the fluid hits the wall at the stagnation-point, the flow is divided into two equal and opposite forces. In the potential flow region, the velocity distribution is assumed as , where is a positive constant. The porous medium has isotropic, homogeneous, and thermodynamic equilibrium with local fluid. Therefore, the governing equations are given by Subject to the boundary conditions the medium is taken to be gray, and emitting radiation and heat flux in the equation of energy due to thermal radiation are given by means of the Rosseland approximation: