# On double-diffusive convection and cross diffusion effects on a horizontal wavy surface in a porous medium

- M Narayana
^{1}, - P Sibanda
^{1}Email author, - SS Motsa
^{1}and - PG Siddheshwar
^{2}

**2012**:88

**DOI: **10.1186/1687-2770-2012-88

© Narayana et al.; licensee Springer 2012

**Received: **6 February 2012

**Accepted: **20 July 2012

**Published: **6 August 2012

## Abstract

An analysis of double diffusive convection induced by a uniformly heated and salted horizontal wavy surface in a porous medium is presented. The wavy surface is first transformed into a smooth surface via a suitable coordinate transformation and the transformed nonsimilar coupled nonlinear parabolic equations are solved using the Keller box method. The local and average Nusselt and Sherwood numbers are given as functions of the streamwise coordinate and the effects of various physical parameters are discussed in detail. The effects of the Lewis number, buoyancy ratio, and wavy geometry on the dynamics of the flow are studied. It was found, among other observations, that the combined effect of Dufour and Soret parameters is to reduce both heat and mass transfer.

**MSC:**34B15, 65N30, 76M20.

### Keywords

double diffusive convection nonsimilar solutions porous medium Keller box method## 1 Introduction

The study of double-diffusive convection has received considerable attention during the last several decades because of its occurrence in a wide range of natural and technological settings. Double-diffusive convection is an important fluid dynamic phenomenon that involves motions driven by two different density gradients diffusing at different rates (Mojtabi and Charrier-Mojtabi [1]). A common example of double diffusive convection is seen in oceanography, where heat and salt concentrations exist with different gradients and diffuse at differing rates. Double diffusive convection manifests in the form of “salt-fingers” (see Stern [2, 3]) which are observable in laboratory settings. The input of cold fresh-water from an iceberg can affect both of these variables. Double-diffusive convection has also been cited as being important in the modeling of solar ponds (Akbarzadeh and Manins [4]) and magma chambers (Huppert and Sparks [5], Fernando and Brandt [6]). Double-diffusive free convection is also seen in sea-wind formations, where upward convection is also modified by Coriolis forces. This is of particular interest in oceans where the Earth’s rotation plays a dominant role in many of the motions observed.

In engineering applications, double diffusive convection is commonly visualized in the formation of microstructures during the cooling of molten metals, and fluid flows around shrouded heat-dissipation fins. Typical technological motivations for the study of double-diffusive convection range from such diverse fields as the migration of moisture through air contained in fibrous insulations, grain storage systems, the dispersion of contaminants through water-saturated soil, crystal growth, solidification of binary mixtures, and the underground disposal of nuclear wastes. Other important applications can be found the fields of geophysical sciences and electrochemistry. A comprehensive review of the literature concerning natural convection in fluid-saturated porous media may be found in the books by Ingham and Pop [7, 8], Nield and Bejan [9], Vafai [10, 11], and Vadasz [12].

Most free convection studies mainly focus on the cases where the thermal boundary conditions allow the use of similarity transformations to reduce the governing boundary layer equations to a system of ordinary differential equations which can be handled either analytically or numerically. The existence of self-similar solutions point to the fact that, in general, the heated surface must have a plane geometry. In reality, the heated surfaces need not always be planar. Surfaces are sometimes deliberately roughened to achieve enhanced heat transport. Heat transfer devices like flat-plate solar collectors and flat-plate condensers in refrigerators possess a nonuniform surface. Further, in cavity wall insulating systems and grain storage systems, one can witness pronounced surface roughness. Yao [13] and Moulic and Yao [14, 15] were the first to include the effects of surface nonuniformities on the free convection thermal boundary layer flow of a Newtonian fluid. Rees and Pop [16, 17] investigated parallel thermal boundary layers due to natural convection induced by a vertical surface with sinusoidal undulations embedded in a in porous medium. Subsequent studies by Rees and Pop [18, 19] considered the effect of surface waves on the convection due to either horizontal or vertical wavy surfaces embedded in a porous medium. In the case of horizontal wavy surface, Rees and Pop [18] found that the amplitude of the surface waves must be within an $O({\mathit{Ra}}^{-1/3})$ range in order to balance direct and indirect buoyancy forces. They showed that for wall amplitudes greater than about $0.95{\mathit{Ra}}^{-1/3}$, the flow separates with one or more regions of reverse flow. Rees and Pop [19] obtained similarity solutions for the case of longitudinal surfaces waves with (i) a prescribed power-law temperature is set on the surface, and (ii) a prescribed power-law heat flux.

Cheng [20–23], in a series of papers investigated free convection due to vertical/inclined wavy surfaces in porous media. Cheng [20] studied natural convection, heat and mass transfer near a vertical wavy surface with constant wall temperature and concentration in a porous medium. He showed that the average Nusselt and Sherwood numbers for a sinusoidal wavy surface are constantly smaller than the corresponding results for a flat plate. This work was generalized in Cheng [21] to a non-Darcy model for natural convection heat and mass transfer from a vertical wavy surface in a porous media. Cheng [22] considered a non-Newtonian power law liquid to study combined heat and mass transfer in free convection flow due to a vertical wavy surface in a porous medium with thermal and mass stratifications. It was found that an increase in the power-law index, the thermal stratification parameter, or the concentration stratification parameter leads to a smaller fluctuation of the local Nusselt and Sherwood numbers with the streamwise coordinate. Double diffusive natural convection along an inclined wavy surface in a porous medium was investigated by Cheng [23] and showed that the inclination angle enhanced the total heat and mass transfer rates.

Pop and Na [24] studied natural convection due to a frustum of a wavy cone in a porous medium and discussed the effects of geometry of a wavy cone on the heat transfer. Cheng [25] studied the natural convection heat and mass transfer near a wavy cone with constant wall temperature and concentration in a porous medium. Using a cubic spline method of solution, he showed that the buoyancy ratio leads to higher heat and mass transports while the diffusivity ratio (Lewis number) reduces heat while increasing mass transports. Cheng [26] obtained nonsimilar solutions for double diffusive convection near a frustum of a wavy cone in porous media and showed that the average Nusselt and Sherwood numbers for the wavy cone are smaller than the corresponding smooth cone. Double-diffusive natural convection along a vertical truncated wavy cone in non-Newtonian fluid saturated porous media with thermal and mass stratification has been investigated by Cheng [27]. In this study, he showed that the power-law index leads to smaller fluctuations in the local Nusselt and Sherwood numbers and increasing the thermal and concentration stratification parameters reduce the heat and mass transfer rates.

An energy flux is often generated by both temperature and solute gradients leading to Dufour or diffusion-thermo effect and Soret or thermal-diffusion effects. Both effects have been extensively studied in gases, while the Soret effect has been studied both theoretically and experimentally in liquids; see Mortimer and Eyring [28]. It is generally accepted that the Dufour and the Soret effects are small compared to the effects described by Fourier and Fick’s laws (Mojtabi and Charrier-Mojtabi [1]) and can therefore be neglected in many heat and mass-transfer processes. However, it has been shown in a number of studies that there are exceptions in areas such as in geosciences where Dufour and Soret effects are significant and cannot be ignored; see for instance Kafoussias and Williams [29], Awad *et al.* [30], and the references therein.

Mortimer and Eyring [28] used an elementary transition state approach to obtain a simple model for Soret and Dufour effects in thermodynamically ideal mixtures of substances with molecules of nearly equal size. In their model, the flow of heat in the Dufour effect was identified as the transport of the enthalpy change of activation as molecules diffuse. The results were found to fit the Onsager reciprocal relationship, Onsager [31]. Shariful *et al.* [32] investigated the Dufour and Soret effects on steady combined free-forced convective and mass transfer flow past a semi-infinite vertical flat plate of hydrogen-air mixtures. They used the fourth-order Runge-Kutta method to solve the governing equations of motion. Their study showed that the Dufour and Soret effects should not be neglected. Shateyi *et al.* [33] investigated the effects of diffusion-thermo and thermal-diffusion on MHD fluid flow over a permeable vertical plate in the presence of radiation and hall current. Recently, Narayana *et al.* [34] and Malashetty and Biradar [35] have investigated the cross diffusion effects on the onset of double diffusive convection in a binary Maxwell fluid saturated porous medium. Other related recent studies on the effects of Soret and Dufour parameters include those by Makinde [36–38].

In this paper, we extend the work by Rees and Pop [18] to include the solute diffusion in natural convection induced by a horizontal wavy surface profile in a porous medium. The wall temperature and concentrations are assumed to be constants and the amplitude of the wave is assumed to be small enough so as not to engender any regions of reverse flow (these issues are dealt in detail by Rees and Pop [18]). Assuming the Rayleigh number *Ra* to be very large, the boundary layer approximation is invoked leading to a set of nonsimilar parabolic partial differential equations whose solution is obtained using the Keller box method (see, Keller [39], Keller and Cebeci [40]).

## 2 Mathematical formulation

*l*is the characteristic length of the wave, and

*φ*is the phase of the wave.

*K*is permeability of the porous medium,

*ν*is the kinematic viscosity,

*β*is the coefficient of thermal expansion, ${\beta}^{\ast}$ is the coefficient of solutal expansion,

*κ*is the thermal diffusivity,

*D*is the solutal diffusivity, ${k}_{1}$ and ${k}_{2}$ are the coefficients of cross diffusion. We now use the following nondimensional variables:

*Ra*, the buoyancy ratio

*N*, Dufour number ${D}_{f}$, the Soret number

*Sr*, and the Lewis number

*Le*defined as follows:

*x*are given by

## 3 Solution procedure

The nonsimilar parabolic partial differential equations that govern the dynamics of the fluid flow were solved using the Keller box implicit finite difference method. This section gives details of the Keller box scheme used to solve the coupled nonlinear parabolic equations (21)-(23). We present the implementation of the Keller box method for a problem that involves coupling, nonlinearity, variable coefficients. The method consists of four main steps; decomposition, discretization, linearization, and the solution of the linearization difference equation.

*ξ*-

*η*plane) is divided into a finite number of mesh points that form the corners of the rectangle shown in Figure 2(a). The net points are defined as

*ξ*and

*η*directions. The choice of net spacings is done manually in the present paper but can be generated automatically. A typical mesh rectangle over which Eqs. (27)-(32) are to be approximated is indicated in Figure 2(b). The equations are centered around one of the points marked by “×.”

*w*we use the following finite difference approximations:

where ${\zeta}_{j}^{i}=\frac{{k}_{j}}{2}[\frac{2}{3}{\eta}_{j-\frac{1}{2}}+\alpha \pi cos(\pi {\xi}_{i-\frac{1}{2}}-\phi ){\xi}_{i-\frac{1}{2}}^{1/3}]$, ${({\chi}_{1})}_{j}^{i}=\frac{{k}_{j}{\xi}_{i-\frac{1}{2}}}{{h}_{i}}$, ${({\chi}_{2})}_{j}^{i}=\frac{\lambda {k}_{j}{\xi}_{i-\frac{1}{2}}}{4{h}_{i}}$, ${({\chi}_{3})}_{j}^{i}=\frac{\lambda {k}_{j}}{4}(\frac{{\xi}_{i-\frac{1}{2}}}{{h}_{i}}+\frac{1}{6})$ and ${({\chi}_{4})}_{j}^{i}=\frac{\lambda {k}_{j}}{2}(\frac{{\xi}_{i-\frac{1}{2}}}{{h}_{i}}-\frac{1}{6})$.

The difference equations (42)-(47) are imposed at each grid points ${\eta}_{j}$, $j=1,2,\dots ,J$ giving rise to 6*J* algebraic equations. The boundary conditions (48) along with the difference equations (42)-(47) comprises a system of $6J+6$ equations for as many variables. There are several methods for solving these $6J+6$ equations. In this study, we employ Newton’s method which is easy to implement.

*n*th iterates of the variables are known the iterate ($n+1$)th iterates are given by

*δ*, the linearized finite difference equations can be written as:

where *I* is an identity matrix of order 6. The procedure involves two sweeps, *i.e.*, a forward sweep and a backward sweep. In the forward sweep, the unknowns ${\mathrm{\Gamma}}_{j}$, ${\mathrm{\Lambda}}_{j}$, and the intermediate variables ${\mathrm{\nabla}}_{j}$ are determined and in the backward sweep the required solution ${\mathrm{\Delta}}_{j}$ is determined in terms of ${\mathrm{\Lambda}}_{j}$ and ${\mathrm{\nabla}}_{j}$.

### Forward sweep

### Backward sweep

After obtaining the solution of the linearized system, the corrections are added to the solutions at the *n* th iteration and the procedure is repeated until convergence is achieved. This gives the solution at a given ${\xi}_{i}$. The procedure is to be repeated at the next streamwise location ${\xi}_{i+1}$ and so on. In boundary layer flows, the greatest error is associated with the wall gradients ${f}_{\eta}(\xi ,0)$, ${\theta}_{\eta}(\xi ,0)$, and ${\varphi}_{\eta}(\xi ,0)$, and hence these are used to determine convergence. The iterations are stopped when the successive iterate values of the gradients match up to 10^{−6}. Since Newton’s method has second-order convergence, usually three to four iterations suffice to achieve the chosen tolerance.

## 4 Results and discussion

Figure 3 shows the cross diffusion effects on the velocity, temperature, and concentration profiles for different values *ξ*. Due to the wavy nature of the surface, the dynamics of the fluid flow at different stream wise locations will be different. We notice the existence of locations where the velocity of the fluid attain extreme values over every undulation of the wavy surface. The profiles are shown for two selected stream wise locations, namely, $\xi =1$ and $\xi =5$. At both of these locations, the effect of cross diffusion is to increase both transverse and axial velocity profiles. The thermal and concentration boundary layers also thicken as a result of the cross diffusion phenomena as can be seen from Figures 3(c) and (d).

*ξ*is shown for different wave amplitudes in Figure 4. For $\alpha =0$, the slip velocity remains constant indicating that self-similar solution exists in the plane surface case. For $\alpha \ne 0$, the slip velocity is oscillatory, increasing first to a maximum before decreasing to a minimum before the cycle is repeated. The fluctuations in the slip velocity increase with increasing amplitudes.

*α*. The local Nusselt number ${\mathit{Nu}}_{x}{\mathit{Ra}}^{-1/3}$ remains smooth and increases with

*ξ*for the plane surface ($\alpha =0$). For the wavy surface ($\alpha \ne 0$), the local Nusselt number fluctuates over every cycle and these fluctuations rise as

*ξ*increases. The fluctuations in the local Nusselt number increase with the wave amplitude. The mean Nusselt number ${\mathit{Nu}}_{m}{\mathit{Ra}}^{-1/3}$ increases with the stream position

*ξ*and with increasing amplitude values.

Figures 5(c) and (d) highlight the mass transfer results for different values of *α*. Analogous to the heat transfer case, the local Sherwood number ${\mathit{Sh}}_{x}{\mathit{Ra}}^{-1/3}$ increases with *ξ* in the case of a plane surface ($\alpha =0$) while for a wavy surface ($\alpha \ne 0$) the local Sherwood number fluctuates. These fluctuations increase as *ξ* increases. Further, the fluctuations in the local Sherwood number increases with the wave amplitude. Figure 5(d) shows that the mean Sherwood number ${\mathit{Sh}}_{m}{\mathit{Ra}}^{-1/3}$ further increases with the stream position *ξ* and with increasing values of *α*. These results are qualitatively similar to those of Rees and Pop [18].

*Le*and the buoyancy ratio

*N*on the slip velocity. The Lewis number reduces the slip velocity while the buoyancy ratio has an enhancing effect as expected. Increasing aiding buoyancy generates faster moving fluid flow as is evident in Figure 6(b).

*N*on the local and mean Nusselt and Sherwood numbers. It is evident that the buoyancy ratio enhances both the local and mean heat and mass transfer coefficients. The buoyancy ratio enhances the local and the mean Nusselt numbers. As observed earlier, ${\mathit{Nu}}_{x}{\mathit{Ra}}^{-1/3}$ and ${\mathit{Sh}}_{x}{\mathit{Ra}}^{-1/3}$ exhibits fluctuations which rise with the streamwise coordinate

*ξ*. These results are in agreement with those reported by Cheng [21] with respect to a vertical wavy surface.

*Le*on the local and mean Nusselt and Sherwood numbers. The Lewis number tends to reduce the local and average heat transfer rates. Further, ${\mathit{Nu}}_{x}{\mathit{Ra}}^{-1/3}$ and ${\mathit{Sh}}_{x}{\mathit{Ra}}^{-1/3}$ exhibit fluctuations which increase with the streamwise coordinate

*ξ*. These results regarding the heat and mass transfer coefficients coincide with those reported by Cheng [21] with respect to the vertical wavy surface. The effect of cross diffusion coefficients on the slip velocity is shown in Figure 9. The slip velocity ${f}_{\eta}(\xi ,0)$ is higher in the presence of cross diffusion effect as compared to the case when cross diffusion effect is absent.

## 5 Conclusions

The paper analyzed double diffusive convection induced by a horizontal wavy surface embedded in a porous medium taking the cross diffusion effect into account. The governing parabolic partial differential equations have been solved using the Keller box method. The convergence rate depends on the parametric values chosen. Computations show that the Lewis number enhances mass transfer while reducing heat transfer. The buoyancy ratio enhances both the heat and mass transfer rates. The surface geometry also plays a crucial role in controlling heat and mass transfer rates. The effect of the Dufour number is to reduce heat transfer and enhance mass transfer. The effect of the Soret number is the exact opposite of the Dufour effect. We observe reduced heat and mass transfer in the presence of cross diffusion terms.

## Declarations

### Acknowledgements

The authors are grateful to the National Research Foundation (NRF) and the University of KwaZulu-Natal for financial support.

## Authors’ Affiliations

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