MHD natural convection from a heated vertical wavy surface with variable viscosity and thermal conductivity.
Choudhury, M. ; Hazarika, G.C. ; Sibanda, P. 等
Introduction
Solutions for the flow over a specified wavy surface are desirable
for understanding the process of wave growth under the action of wind
and the effects of surface configuration on drag (Caponi et. al [3]).
Solutions for flow over small amplitude wavy surfaces were obtained by
Miles [17] and by Benjamin [1]. Lyne [15] used the method of conformal transformation to investigate the steady streaming generated by an
oscillatory viscous flow over a wavy wall. One of the reasons why a
roughened surface is more efficient in heat transfer is its capability
to promote fluid motion near the surface. Among others, Moulic and Yao
[18] studied natural convection along a wavy surface with uniform heat
flux. Yao [27] concluded that total heat transfer rate for a wavy
surface of any kind, in general, is greater than that of a flat surface.
Since the work of Schmidt and Beckman [23], the study of natural
convection has been one of the most important research topics in heat
transfer problems. The problem of natural or mixed convection along a
sinusoidal wavy surface has received considerable attention because such
a surface can be viewed as an approximation to certain geometries of
practical relevance in heat transfer [2, 26, 27].
Fluid viscosity and thermal conductivity (hence thermal
diffusivity) play an important role in the flow characteristic of
laminar boundary layer problems. Fluid properties are significantly
affected by the variation of temperature. The increase in temperature
leads to a local increase in the transport phenomena by reducing the
viscosity across the momentum boundary layer and so the heat transfer
rate at the wall is affected. In the cooling of electronic equipments,
it is relatively frequent to find circumstances in which variable
property effects are significant and cannot be neglected.
Sparrow and Gregg [24] was the first to study the variable fluid
property in natural convection. Later, Zhong et. al [29], Kafousias and
Williams [13], Zamora and Hernandez [28], Hernandez and Zamora [9] and
Maleque and Sattar [16] considered variable property effects on natural
convection flow. Hazarika and Lahkar [8] observed that a significant
variation takes place in velocity and temperature distribution with the
variation of the viscosity and thermal conductivity parameters. Hossain
et. al [10] studied natural convection of fluid with variable viscosity
from a heated vertical wavy surface.
Magnetoconvection plays an important role in many industrial
applications. Such flows also occur naturally in geophysical and
astrophysical problems during the cooling or heating of liquid metals
(Nagata [19]). The presence of a magnetic field may, in some instances,
have the effect of limiting the effectiveness of cooling systems by
increasing wall temperatures, Sharma and Singh [22], Uda et. al.[25].
The application of a magnetic field suitably oriented to the flow in a
shock layer may modify the flow pattern and this in turn may cause a
change in the heat transfer characteristics of the body, Gupta et. al
[7]. A magnetic field applied transverse to the plate causes a reduction
in heat transfer at the plate (Gupta [6]). Hossain et.al. [11] studied
magnetohydrodynamic free convection along a vertical wavy surface.
Hossain and Pop [12] investigated the magnetohydrodynamic boundary layer
flow and heat transfer from a continuous moving wavy surface.
The aim of this paper is to study the effects of temperature
dependent viscosity and thermal conductivity on natural convection flow
of a viscous incompressible electrically conducting fluid from a
vertical wavy surface. The flow is subject to a uniform transverse
magnetic field. Both the fluid viscosity and thermal conductivity vary
as inverse linear functions of temperature. Recent studies of a similar
nature with temperature dependent viscosity and thermal conductivity
have been carried out by, among others, Sharma and Singh [22] for flow
along a vertical non-conducting plate with internal heat generation and
by Rahman et. al. [21] for MHD natural convection of an electrically
conducting fluid, also along a vertical flat plate. The recent study by
Prasad et. al. [20] considered the MHD flow of a viscoelastic fluid and
heat transfer over a stretching sheet. The effect of
temperature-dependent viscosity on heat transfer over a continuous
moving surface had earlier been considered by Elbashbeshy and Bazid [5].
Formulation of the problem
Consider the steady laminar free convective boundary layer flow of
a viscous incompressible electrically conducting fluid from a
semi-infinite vertical wavy surface. The geometric model considered is a
wavy surface similar to that in Hossain et al. [10] and shown
schematically in Fig. 1.
The [bar.x]--axis is taken along the vertical surface in the flow
direction and the [bar.y] axis normal to the surface. The flow is
subject to a uniform magnetic field of strength [B.sub.0] applied
transverse to the direction of the flow. The plate is electrically
non-conducting. The surface temperature is held uniform at [T.sub.w]
warmer than the ambient temperature [T.sub.[infinity]] .The surface
modulation is described by [bar.y] = [bar.[sigma]]([bar.x])
where [bar.[sigma]] is a surface geometry function. The
mathematical formulation proposed in Hossain et. al. [10] allows
[bar.[sigma]] to be of arbitrary shape but a sinusoidal surface was used
as an example in the computations. The sinusoidal profile of the wavy
surface is given by [[bar.[sigma]].sub.x] = [alpha] sin x where [alpha]
is an amplitude function.
[FIGURE 1 OMITTED]
Following Lai and Kulacki [14], the fluid viscosity is assumed to
be an inverse linear function of the temperature T of the form;
[mu] = [[mu].sub.[infinity]]/[1 + [gamma](T-[T.sub.[infinity]])] or
1/[mu] = a (T-[T.sub.r]) (1)
where a = [gamma]/[[mu].sub.[infinity]] and [T.sub.r] =
[T.sub.[infinity]] -1/[gamma], is the fluid temperature, [mu] is the
coefficient of dynamic viscosity, [[mu].sub.[infinity]] is the
coefficient of viscosity at the free stream, a, [T.sub.r] and [gamma]
are constants whose values depend on the reference state and the thermal
property of the fluid. In general, for liquids a > 0 and for gases a
< 0. For [gamma] = 0, the fluid viscosity is constant throughout the
flow field.
The variation of thermal conductivity with temperature is
considered to be as follows, see also Hazarika and Lahkar [8];
1/k = [1 + [epsilon](T - [T.sub.[infinity]])]/[k.sub.[infinity]] or
1/k = c (T - [T.sub.k]) (2)
where c = [epsilon]/[k.sub.[infinity]] and [T.sub.k] =
[T.sub.[infinity]] -1/[epsilon], k is the thermal conductivity of the
fluid, [k.sub.[infinity]] is the thermal conductivity of the ambient
fluid, c, [T.sub.k] and [epsilon] are constants whose values depend on
the reference state and the thermal property of the fluid. For liquids c
> 0 while for gases c < 0.
Under the usual Boussinesq approximation (see Rahman et al. [21],
Sharma and Singh [22]), the flow is governed by the following boundary
layer equations
[partial derivation][bar.u]/ [partial derivation][bar.x] + [partial
derivation][bar.v]/[partial derivation][bar.y] = 0 (3)
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII] (4)
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII] (5)
[bar.u] [partial derivation]T/[partial derivation][bar.x] + [bar.v]
[partial derivation]T/[partial derivation][bar.y] = 1/[rho][c.sub.p]
[DELTA] x (k[DELTA]T) (6)
where [bar.u] and [bar.v] are the [bar.x], [bar.y] components of
the velocity field with the bar denoting dimensional quantities,
[[DELTA].sup.2] = [[partial derivation].sup.2]/[partial
derivation][[bar.x].sup.2] + [[partial derivation].sup.2]/[partial
derivation][[bar.y].sup.2], g is the gravitational acceleration, [rho]
is the density of the fluid, [bar.p] is the fluid pressure, [c.sub.p] is
the specific heat at constant pressure, [beta] is the coefficient of
thermal expansion and [B.sub.0] is the applied magnetic field strength.
The boundary conditions are,
[bar.u] = 0, [bar.v] = 0 T = [T.sub.w] at [bar.y] = [y.sub.w] =
[bar.[sigma]]([bar.x]) (7a)
[bar.u] [right arrow] 0, T [right arrow] [T.sub.w] as [bar.y]
[right arrow] [infinity]. (7b)
To non-dimensionalize equations. (3)--(6) we introduce the
following scales;
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII], (8a)
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII], (8b)
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII], (8c)
where Gr is the thermal Grashof number, L is the fundamental
wavelength, p is the dimensionless pressure and [p.sub.[infinity]] is
the ambient pressure, [theta] is the non-dimensional temperature,
[[theta].sub.r] and [[theta].sub.k] are a viscosity measuring parameter
and a transformed dimensionless reference temperature respectively. The
parameter A is a thermal influence parameter (see Cramer and Pai [4])
and M is the Hartmann number. The parameter [[theta].sub.r] is positive
for gases and negative for liquids if [T.sub.w] > [T.sub.[infinity]].
Using the transformations (8a)-(8c) in equations (3)--(6) and
ignoring terms of small orders in the Grashof number Gr we have,
[partial derivation]u/[partial derivation]x + [partial
derivation]v/[partial derivation]y = 0 (9)
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII], (10)
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII] (11)
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII], (12)
where Pr = [[mu].sub.[infinity]][c.sub.p]/[k.sub.[infinity]] is the
Prandtl number. The associated boundary conditions are
u = 0, v = 0, [theta] = 1 on y = 0 (13a) u [right arrow] 0, [theta]
[right arrow] 0 as y [right arrow] [infinity] . (13b)
Equation (11) indicates that the pressure gradient along the
y--direction is O([Gr.sup.1/4]) which implies that the lowest order
pressure gradient along the x-direction can be determined from the
inviscid flow solution.
Eliminating the pressure terms between equations (10) and (11)
gives
[MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII] (14)
From a technological point of view it is important to know the
local skin-friction [C.sub.f] and the local Nusselt number Nu . These
are given in non-dimensional form by
[C.sub.f] = (1 +
[[sigma].sup.2.sub.x][[theta].sub.r]/[[theta].sub.r] - 1
[Gr.sup.3/4][([partial derivation]u/[partial derivation]y).sub.y = 0]
(15)
[N.sub.u] = -(1 + [[sigma].sub.x])[[theta].sub.k]/[[theta].sub.k] -
1 [Gr.sup.1/4] [([partial derivation][theta]/[partial
derivation]y).sub.y = 0]. (16)
Results and Discussions
The system of differential equations (9), (12) and (14) subject to
the boundary conditions (13) was solved numerically. A finite difference
solution is straightforward since the computational grids are fitted to
the shape of the wavy wall. Central differences were used for the
diffusion terms and the forward difference scheme for the convection
terms. After experimenting with a few set of mesh sizes, the mesh sizes
were fixed at [DELTA]x = 0.1and [DELTA]y = 0.01which gave sufficient
accuracy for Pr = 0.7, Grashof number Gr = 0.2 and wave amplitude
[alpha] = 0.2.
Table 1 displays the values of the skin-friction coefficient and
Nusselt number at the surface for different values of [[theta].sub.r].
Increasing the viscosity parameter leads to increases in the values of
both the skin friction coefficient and the heat transfer coefficient.
This finding is similar to the results obtained by Prasad et al. [20] in
their study of the effects of variable viscosity on MHD viscoelastic
flow and heat transfer over a stretching sheet and arises because the
fluid is able to move more easily close to the heated surface since its
viscosity is lower relative to the constant viscosity case.
Table 2 shows the effect of increasing the thermal conductivity
parameter on the skin friction and the heat transfer coefficients when M
= 0.5, Pr = 0.7. The related study by Rahman et al. [21] for flow along
a vertical plate with heat generation used M = 0.10 and Pr = 0.733.The
results are qualitatively similar and show that increasing the thermal
conductivity of the fluid leads to an increase in the skin-friction
coefficient but a decrease in the Nusselt number. This may partly be
explained by the fact that that increasing thermal conductivity has the
effect of accelerating and increasing the temperature of the fluid.
Table 3 shows the effect of increasing the magnetic field intensity
on the skin friction coefficient and the Nusselt number for constant
values of viscosity and thermal conductivity. Simulations show that the
increasing the magnetic field intensity leads to a decrease in the
skin-friction coefficient as well as in the heat transfer coefficient.
This is broadly in line with the recent findings by Sharma and Singh
[22] who also observed that the heat transfer coefficient however
decreases with Prandtl numbers. The study by Rahman et al. [21] however
found that an increase in the magnetic field intensity leads to an
increase in the surface temperature.
The tangential and normal velocity components and the temperature
distributions are displayed in Figs.1-5 for various viscosity, thermal
conductivity and magnetic parameter values. Figs. 1 and 2 depict the
effects of the viscosity variation parameter [[theta].sub.r] on the
tangential and normal velocity components for fixed values of thermal
conductivity parameter [[theta].sub.k] = -15, Hartman number M = 0.5 and
Prandtl number Pr = 0.7. Increases in the values of 0r lead to an
increase in the velocity field away from the surface. This results are
however different to the case of a viscoelastic fluid where Prasad et
al. [20] showed that the velocity decreases with increasing values of
the viscosity parameter. The effect of an increase in the value of this
parameter on the temperature distribution is not significant in the
entire boundary layer region. The velocity and the temperature profiles
for values of the thermal conductivity parameter [[theta].sub.k] = -15,
-12, -9, -5 and viscosity parameter [[theta].sub.r] = -15 are depicted
in Figs. 3 and 4. The results are in line with the findings in Prasad et
al. [20] and show that the velocity and temperature profiles increase
with increases in [[theta].sub.k]. This effect is however not very
significant in the case of the normal velocity component.
[FIGURE 1 OMITTED]
[FIGURE 2 OMITTED]
[FIGURE 3 OMITTED]
[FIGURE 4 OMITTED]
Fig. 5 shows the velocity profiles for Hartman numbers M = 0,5, 10,
uniform
viscosity [[theta].sub.k] = -10 and thermal conductivity and
[[theta].sub.r] = -10. The velocity curves show that the rate of
transport is reduced with increases in M . This clearly confirms that
the transverse magnetic field opposes the transport phenomena confirming
the earlier findings in, for example, Prasad et al. [20], Rahman et al.
[21] and Sharma and Singh [22]. This is because the variation of the
Hartmann number leads to the variation of the Lorentz force due to the
magnetic field and the Lorentz force produces resistance to transport
phenomena.
[FIGURE 5 OMITTED]
Conclusion
We have investigated the effect of temperature-dependent viscosity
and thermal conductivity on the MHD flow of an incompressible
electrically conducting fluid along a semi-infinite vertical plate with
a wavy surface. The study shows that increasing the viscosity variation
leads to increases in both the skin friction and the heat transfer
coefficient. The effect of increasing the thermal conductivity is also
to increase the skin friction while reducing the Nusselt number. Both
the skin friction and the heat transfer coefficients decrease with
increases in the magnetic field parameter. The numerical simulations
thus show that fluid viscosity and thermal conductivity (hence thermal
diffusivity) play an important role in the flow characteristics of
laminar boundary layer problems. Fluid properties are significantly
affected by the variation of the viscosity and thermal conductivity due
to temperature changes. The effects of the Lorentz force due to applied
magnetic field has the effect of retarding the transport phenomena.
Nomenclature
A thermal influence parameter
[B.sub.0] = Magnetic field induction
[C.sub.f] = local skin friction
[C.sub.p] = Specific heat at constant pressure
Gr = Grashof number
g = Acceleration due to gravity
k = Thermal conductivity
L = wavelength
M = Hartmann number
Nu = local Nusselt number
p = fluid pressure
Pr = Prandtl number
T = fluid temperature
[bar.u], [bar.v] = dimensional stream wise and normal velocity
components
[bar.x], [bar.y] = dimensional tangential and normal coordinate
axis
Greek Symbols
[alpha] = surface wave amplitude
[beta] = coefficient of thermal expansion
[gamma], [epsilon] = constants based on the thermal property of the
fluid
[mu] = coefficient of dynamic viscosity
[rho] = fluid density
[bar.[sigma]] = surface geometry function
[upsilon] = coefficient of kinematic viscosity
[theta] = dimensionless temperature term
[[theta].sub.k] = thermal conductivity variation parameter
[[theta].sub.r] = viscosity variation parameter
Subscripts
k, r = reference state values
[infinity] = ambient free-stream values
w = wall surface conditions
References
[1] Benjamin, T. B., (1959) Shearing flow over a wavy boundary, J.
Fluid Mech., 6, pp. 161-205.
[2] Bhavnani, B. H., Bergles, A. E., (1991) Natural convection heat
transfer from sinusoidal wavy surface, Warme and
stoffuebertragung/Thermo fluid dynamics, 26, pp. 341-349, 1991.
[3] Caponi, E. A., Fornberg, B. D., Knight, D., MCLean, J. W.,
Saffman, P. G., Yuen, H. C., (1982) Calculation of laminar viscous flow
over a moving wavy surface, J. FluidMech., 124, pp. 347-362.
[4] Cramer, K. R., Pai, S. T., (1973) Magnetofluid dynamics for
engineering and applied physicists. McGraw-Hill.
[5] Elbashbeshy, E. M .A., Bazid, M. A. A., (2004) The effect of
temperature dependent viscosity on heat transfer over a continuous
moving surface with variable internal heat generation, Appl. Math.
Comput., 153, pp. 721-731.
[6] Gupta, A. S., (1960) Steady and transient free convection of an
electrically conducting fluid from a vertical plate in the presence of a
magnetic field, Appl. Sci. Research (A) 9, pp. 319-333.
[7] Gupta, A. S., Mishra, J. C., Reza, M, (2005) Magneto hydrodynamic shear flow along a flat plate with uniform suction or
blowing, ZAMP 56, pp. 1030-1047.
[8] Hazarika, G. C., Lahkar, J., (1997) Effects of variable
viscosity and thermal conductivity on free convective mass transfer flow
past a vertical isothermal cone surface in presence of magnetic field,
Mathematical Forum, XI.
[9] Hernandez, J., Zamora, B., (2005) Effects of variable
properties and non uniform heating on natural convection flow in
vertical channels, Int. J. Heat and Mass Transfer., 48, pp. 793-807.
[10] Hossain, M. A., Kabir, S., Rees, D.A.S., (2002) Natural
convection of fluid with variable viscosity from a heated vertical wavy
surface, ZAMP, 53, pp. 4852.
[11] Hossain, M. A., Alam, K. C. A., Rees, D. A. S., (1997)
Magnetohydrodynamic free convection along a vertical wavy surface,
Appld. Mech. Engg., 1, pp. 555566, 1997.
[12] Hossain, M. A., Pop, I., (1996) Magnetohydrodynamic boundary
layer flow and heat transfer on a continuous moving wavy surface, Arch.
Mech., 48, pp. 813-823.
[13] Kafousias, N. G., Williams, W., (1995) Thermal- diffusion and
diffusion thermo effects on mixed free-forced convective and mass
transfer boundary layer flow with temperature dependent viscosity, Int.
J. Engng. Sci., 33, pp. 1369-1384.
[14] Lai, F. C., Kulacki, F. A., (1990) The effect of variable
viscosity on convective heat transfer along a vertical surface in a
saturated porous medium, Int. J. Heat Mass Transfer, 33, pp.1028-1031.
[15] Lyne, W. H., (1971) Unsteady viscous flow over a wavy wall, J.
Fluid Mech., 50, pp. 33-48.
[16] Maleque, Kh. A., Sattar, Md. A.,(2005) The effects of variable
properties and Hall current on steady MHD laminar convective fluid flow
due to a porous rotating disk, Int. J. Heat and Mass Transfer, 48, pp.
4963-4972.
[17] Miles, J., (1957) On the generation of surface waves by shear
flows, J. Fluid Mech, 3, pp. 185-204.
[18] Moulic, S. G., Yao, L. S., (1989) Natural convection along a
wavy surface with uniform heat flux, ASME J. Heat Transfer, 111, pp.
1106-1108.
[19] Nagata, M., (1998) Nonlinear analysis on the natural
convection between vertical plates in the presence of a horizontal
magnetic field, Eur. J. Mech., B/Fluids, 17, pp. 33-50.
[20] Prasad, K. V., Pal, D., Umesh, V., Rao, N. S. P., (2010) The
effect of variable viscosity on MHD viscoelastic fluid flow and heat
transfer over a stretching sheet, Commun. Nonlinear Sci Numer Simul, 15,
pp. 331-344.
[21] Rahman, M. M., Mamun, A. A., Azim, M. A., Alim, (2008) M. A.
Effects of temperature dependent thermal conductivity on MHD free
convection flow along a vertical flat plate with heat conduction,
Nonlinear Analysis: Modelling and Control, 13 (4), pp. 513-524.
[22] Sharma, P. R., Singh, G., (2009) Effects of varying viscosity
and thermal conductivity on steady MHD free convective flow and heat
transfer along an isothermal plate with internal heat generation, Int.
J. Numerical Methods for Heat and Fluid Flow, 19, pp. 78-92.
[23] Schmidt, E., Beckman, W., (1930) Tech. Mech. UI. Thermodynam.,
1, pp. 341349.
[24] Sparrow, E. M., Gregg, J. L., (1958) The variable fluid
property problem in free convection, J. Heat Transfer, 80, pp. 879-886.
[25] Uda, N., Hayase, M., Chikaoka, T., Inoue, S., Horiike, H.,
Miyazaki, K., (2000) Natural convective heat transfer of lithium under
magnetic field, Fusion Engineering and Design ,51-52, pp. 893-898.
[26] Yao L. S., (1983) Natural convection along a vertical wavy
surface, ASME J. Heat Transfer, 105, pp. 465-468.
[27] Yao, L. S., (2006) Natural convection along a vertical complex
wavy surface, Int. J. Heat and Mass Transfer, 49, pp. 281-286.
[28] Zamora, B., Hernandez, J., (1997) Influence of variable
property effects on natural convection flows in asymmetrically heated
vertical channels, Int. Comm. Heat Mass Trans., 24, pp. 1153-1162.
[29] Zhong Z. Y., Yang, K. T., Lloyd, J. R., (1985) Variable
property effects in laminar natural convection in a square enclosure, J.
Heat Transfer, 107, pp. 103-138.
M. Choudhury (1) *, G.C. Hazarika (2) and P. Sibanda (3)
(1) Department of Mathematics, N.N.S. College, Titabar,
Assam-785630, India
* Corresponding author E-mail: mirabpgc@gmail.com
(2) Department of Mathematics, Dibrugarh University, Dibrugarh,
Assam-786004, India.
(3) School of Mathematical Sciences, University of KwaZulu-Natal,
Private Bag X01, Scottsville 3209, Pietermaritzburg, South Africa
E-mail: sibandap@ukzn.ac.za
Table 1: Effect of variable viscosity [[theta].sub.r] on the
skin-friction coefficient and Nusselt number when M = 0.5, Pr = 0.7,
[[theta].sub.k] = -15.
[[theta].sub.r] [C.sub.f] Nu
-15 0.027088 -1.90584
-13 0.028313 -1.90318
-11 0.029985 -1.90317
-9 0.032397 -1.90317
-7 0.036184 -1.90311
-5 0.042990 -1.90306
-3 0.058832 -1.90291
-1 0.137251 -1.90223
Table 2: Values of skin-friction coefficient and Nusselt number for
different [[theta].sub.k] and M = 0.5, Pr = 0.7,
[[theta].sub.r] = -15.
[[theta].sub.k] [C.sub.f] Nu
-15 0.027088 -1.071795
-13 0.028155 -1.08392
-11 0.029799 -1.10102
-9 0.032675 -1.127015
-7 0.039155 -1.171557
-5 0.073148 -1.267624
Table 3: Values of skin-friction coefficient and Nusselt number for
different M and [[theta].sub.k] = -10, Pr = 0.7,
[[theta].sub.r] = -10.
M [C.sub.f] Nu
0 0.036579 -3.04150
2 0.036402 -3.04165
4 0.036090 -3.04169
6 0.035575 -3.04176
8 0.034866 -3.04184
10 0.033974 -3.04196