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IOSR Journal of Mathematics (IOSR-JM)
e-ISSN: 2278-5728,p-ISSN: 2319-765X, Volume 7, Issue 2 (Jul. - Aug. 2013), PP 76-87
www.iosrjournals.org
www.iosrjournals.org 76 | Page
Effects Of Heat Source And Thermal Diffusion On An Unsteady
Free Convection Flow Along A Porous Plate With Constant Heat
And Mass Flux In A Rotating System Under Slip Boundary
Condition
Hoshiyar Singh1
, N.C. Jain2
and D. Chaudhary3
1
Department of Mathematics, Jaipur National University Jagatpura, Jaipur-302025, Rajasthan (India)
2
Department of Mathematics, University of Rajasthan, Jaipur-302055, Rajasthan (India)
Abstract: The present analysis is made to investigate the effects of heat source and thermal diffusion on an
unsteady free convection flow along a porous vertical plate in a rotating system. The plate is subjected to
constant heat and mass flux also. The problem is solved analytically and expressions for velocity. Energy and
temperature profiles, skin friction and Nusselt number are obtained. The effects of different parameter entered
in the problem are discussed on the primary and secondary velocities, temperature and concentration
distributions, primary and secondary skin frictions and Nusselt number with the help of tables and graphs.
Key Words: Diffusion, Heat Source, Porous Medium, Slip Velocity, Unsteady Flow.
I. Introduction
The flow through a porous medium is a common occurrence in industrial environment and so the heat
transfer problems of viscous incompressible fluid through a porous medium has attracted the interest of many
research workers in view of its applications in geophysics, astrophysics, aerodynamics, boundary layer control
and so on.
A number of authors such as Soundalgekar et al. [1], Raptis and Perdikis [2], Mohammad [3], Helmy
[4] and recently Jain and Gupta [5] have investigated flow through porous medium on different geometries. The
effect of variable permeability on combined free and forced convection in porous media was studied by
Chandrasekhara and Namboodiri [6] and Mixed Convection in porous media with uniform heat flux on vertical
surface was studied by Joshi and Gebhart [7]. Lai and Kulacki [8] studied the effect of variable viscosity along a
vertical surface in a saturated porous medium.
The phenomena of heat and mass transfer is encountered in chemical process industries such as food
processing and polymer products. Raptis and Kafousias [9], Bejan and Khair [10], Elbashbeshy [11], Acharya et
al. [12], Chand et al. [13] are some of the workers to study the different problems through porous medium with
mass transfer effects.
In high attitude flights, situation may arise when the flow becomes unsteady and slip at the boundary
take place as well. In such situation of slip flow ordinary continuum approach fails to yield satisfactory result
[Tsien [14], Street [15]]. Many authors have solved problems taking slip conditions at the boundary. Recently
Jothimani and Anjali Devi [16], Jain et al. [17] and Gupta et al. [18] have considered slip boundary conditions in
their problems.
In the present work we study the effects of heat source and permeability on unsteady free convection
rotating flow of a viscous fluid past a porous vertical plate with time dependent suction and velocity slip
boundary conditions. At the plate there is constant heat flux and mass flux. Perturbation technique is used to
obtain the expressions of velocity and temperature fields, concentration profile, skin friction and Nusselt
number. Effects of different parameters viz. Grashoff number of heat transfer, Grashoff number for mass
transfer, slip parameter, permeability parameter, heat source parameter, Diffusion parameter and Schmidt
number are discussed and shown graphically. It is observed that increase in Schmidt number decreases primary
skin friction (p) as well as secondary skin friction (s) while increase in Grashoff number increase both the skin
fictions. Moreover, increase in Prandtl number decreases Nusselt Number (Nu).
II. Mathematical Formulation
We consider an unsteady free convection flow of an incompressible viscous fluid through a porous
medium past an infinite vertical porous plate with constant heat and mass fluxes. Let both the fluid and plate be
in a state of rigid rotation with uniform angular velocity  about z-axis taken normal to the plane and plate is
taken electrically non-conducting. Moreover the plate is assumed to coincide with the plane z = 0. As the plate is
infinite in extent and the flow is unsteady, all the physical variables depend on z and t only.
77Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 77 | Page
For the governing equations for a free convective flow with heat source along a porous vertical plate in
rotating system are given as:
Continuity equation
0
z
w



…(2.1)
Momentum equations
u
K
C(C'gTTg
z
u
v2
z
u
w
t
u
2
2











…(2.2)
v
Kz
v
u2
z
v
w
t
v
2
2










…(2.3)
Energy equation














TT
C
S
z
T
Cz
T
w
t
T
p
*
2
2
p
…(2.4)
Concentration equation
2
2
2
2
z
T
D
z
C
D
z
C
w
t
C












…(2.5)
Here  is the density, g is the acceleration due to gravity,  is the coefficient of volume expansion,
'
 is
the coefficient of concentration expansion,  is the kinematic viscosity, T is the temperature of the fluid in the
free stream, C is the concentration at infinite, u and v are the velocities in x and y direction respectively, T is
the temperature of the fluid, K is the permeability of porous medium,  is the thermal conductivity, D is the
concentration diffusivity, Cp is the specific heat at constant pressure, S*
is the coefficient of heat source, Dℓ is
coefficient of diffusivity.
The boundary conditions are:






















zasCCTT0,v0,u
0zat
D
m'
z
Cq'
z
T
z
v
Lv
z
u
Lu
…(2.6)
Here q' and m' are uniform heat and concentration flux at the plate respectively, L being Mean free path.
Integration of equation (2.1) gives:
 nt
0
e1ww …(2.7)
Using equation (2.7) and introducing following non-dimensional quantities



tw
t,
w
n
n,
wz
z,
w
v
v,
w
u
u
2
0*
2
0
*0*
0
*
0
*

2
2
0*00
K w
K
m'
DwCC
q'
wTT







 
(Permeability parameter)



p
C
Pr (Prandtl number),
D
Sc

 (Schimdt number)
2
0
w
E

 (Rotation velocity parameter),
2
0
2
*
w
S
S


 (Heat Source parameter)
78Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 78 | Page


 4
0
2
w
q'g
Gr (Grashoff number for heat transfer),
Dw
m''g
Gm 4
0
2

 (Grashoff number for mass transfer)
m'
Dq'
A

 
(Diffusion parameter),

 0
wL
h (slip parameter) …(2.8)
Equations (2.2) to (2.5) reduce to the following form after dropping the asterisks over them:














 
GmGr
K
1
s
t
q
z
q
e1
z
q nt
2
2
…(2.9)








 
S
t
Pr
z
e(1Pr
z
nt
2
2
…(2.10)
t
Sc
z
e(1Sc
z
nt
2
2







 
2
2
z
A


 …(2.11)
where q = u +iv and s = 2iE.
The corresponding boundary conditions become:















zas000,q
0zat1
z
1
zz
q
hq
…(2.12)
III. Solution Of The Problem
To solve equations (2.9) to (2.11), we follow the perturbation technique in the form ( < < 1)
  2
2
nt
1
0(z)qez)qq …(3.1)
  2
2
nt
1
(0z)ez) …(3.2)
  3
2
nt
1
0(z)ez) …(3.3)
Substitution of Equations (3.1) to (3.3) in Equations (2.9) to (2.11) and equating the coefficient of like
powers of  (neglecting 2
etc.), we obtain the following set of differential equations
111
1
2
1
2
GmGrq
k
1
s
dz
dq
dz
qd






 …(3.4)
dz
dq
GmGrq
K
1
sn
dz
dq
dz
qd 1
212
1
2
2
2






 …(3.5)
1
1
2
1
2
S
dz
d
Pr
dz
d




…(3.6)
dz
d
PrS)Prn
dz
d
Pr
dz
d 1
2
2
2
2
2





…(3.7)
79Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 79 | Page
0
dz
d
A
dz
d
Sc
dz
d
2
1
2
1
2
1
2






…(3.8)
2
2
2
1
2
2
2
2
2
dz
d
A
dz
d
ScScn
dz
d
Sc
dz
d 






…(3.9)
the corresponding boundary conditions are:















zas00000q0q
0zat0
dz
d
1
dz
d
0
dz
d
1
dz
d
dz
dq
hq
dz
dq
hq
212121
21212
2
1
1 …(3.10)
On solving equations (3.4) to (3.9) under the transformed boundary conditions (3.10), we get the
solution for ,  and q as follows

 z2D
2
z1D
1
ntz1D
1
eReRee
D
1
…(3.11)

 z3D
8
z2D
7
z1D
6
zSc
5
ntz1D
4
zSc
3
eReReReReeReR …(3.12)
z3D
19
z2D
18
z1D
17
ntz4D
11
zSc
10
z1D
9
eReReReeReReRq



 z5D
22
zSc
21
z4D
20
eReReR …(3.13)
Using q = u+iv, the expressions for the primary and secondary velocities are obtained as follows
z1A
2
nt
20102
nt
199
ez}AsineK(KzAcoseK(K{[t)u(z,


z1Dnt
131
z3Ant
426425
eeKKeez)sinAKzAcosK


  zScnt
213
z3Dnt
17
z2Dnt
15
eeKKeeKeeK …(3.14)
z1A
2
nt
1992
nt
2010
ez}AsineKKzAcoseK[{(Kt)v(z,


z1Dnt
142
z3Ant
426425
eeKKeez)AcosKzAsinK


  zScnt
224
z3Dnt
18
z2Dnt
16
eeKKeeKeeK …(3.15)
IV. Skin Friction And Heat Transfer
Once the expressions for velocities and temperature are known it is important to calculate the skin-
friction and Nusselt number. The skin friction p is due to primary velocity u and skin friction s is due to
secondary velocity v in the x and y directions respectively.
The coefficient of skin friction in x and y directions are:








 

2
nt
20101
nt
199
0z
x
AekkAekk
z
u
 
311
nt
21173152131426325
kSckDekSckDkDkDAkAk
…(4.1)








 

2
nt
1991
nt
2010
0z
y
AekkAekk
z
v
80Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 80 | Page
 
421
nt
22183162141425326
kSckDekSckDkDkDAkAk
…(4.2)
and the rate of heat transfer is given by
nt
211
1
eRRD1
D
t)0,
1
Nu 



 …(4.3)
where
2
b'
A
2
a'1
A
2
b
A
2
a1
A 4321





21
121221
2
K4164E4K{(1
a







 

21
121221
2
K4164E4K{(1
b







 

21
121221
2
4nK4164E4n4K{(1
a'







 

21
121221
2
4nK4164E4n4K{(1
b'







 




2
4SPrPr
D
2
1



2
S)Pr4(nPrPr
D
2
2



2
Sc4nScSc
D
2
3




2
2iE)K411
D
1
4
2
2iE)nK411
D
1
5






S)PrnDPrD
Pr
R
1
2
1
1
2
11
2 D
DR
R  ,




Sc)(DSc
ScA)1D
R
1
1
3



ScD
A
R
1
4

n
ScR
R 3
5




nScScDD
DRAScDR
R
1
2
1
2
1114
6



ScnDScD
DAR
R
2
2
2
2
22
7



3
27165
8 D
DRDRScR
R
 109114310219
iKKRKiKRiKKR
 81472136512
RGmRRGmRGrRiKKR
81Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 81 | Page
 1615181413178716121115
iKKRiKKRiKKRiKKR
 262522222121201920181719
iKKRKiKRiKKRiKKR



 

221
1
2
1
2
1
1
1
2
141
1
4EKDDD
KDDRGmDGr
K 


  221
1
2
1
2
1
41
2
4EKDDD
RGmD(Gr2E
K



 

2212
3
12
3
4EKScSc
RGmKScSc
K 

  2212
3
4
4EKScSc
RGm2E
K
 11515
DKRGmRGrK  126
DKK
 357
KScRGmK  48
KScK










 2
2
22
1
41223111
9
AhAh(1
Sc)]h1KhD1KAhSc)]h1KDh1KAh1
K ,










 2
2
22
1
31124121
10
AhAh(1
Sc)h1KDh1KAhSc)]h1KDh1KAh1
K ,
 1029111
KARAK  1019212
KARAK









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82Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 82 | Page
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V. Discussion And Conclusions
In order to get physical insight of the problem, calculations have been made for primary and secondary
velocities (u,v), temperature (), concentration (), primary and secondary skin-frictions (p,s) and Nusselt
number (Nu) for different parameters viz. Prandtl number (Pr), Schmidt Number (Sc), Permeability parameter
(K). Heat source parameter (S), Grashof number for heat transfer (Gr), Grashof number for mass transfer (Gm),
Diffusion parameter (A) and Slip parameter (h) fixing  = 0.02, E = 0.4, n = 0.1 and t = 1.0.
From Figure 1, important observation is that increase in h, increases the primary velocity near the plate
but after some distance it decreases Physically it due to the fact that effect of slip parameter nullify as we go far
from the plate. However, in case of Gm and S velocity increases as both the parameters decreases but Gr has
opposite phenomena. From Figure 2, for secondary velocity v (in the figure we have plotted – v ) the
observations are same as that of primary velocity for the case of Gr, Gm and S but interestingly as h increases
secondary velocity decrease near the plate but goes on increasing as we move away from the plate.
In figure 3 and 4 the primary and secondary velocities u and v are plotted for different values of Pr, K
and Sc. From the figures we observed that an increase in Pr and Sc decreases primary but increases secondary
velocity. It is further observed that for increasing K both velocities (u,v) increases. Physically, we say that
increase in K increases the flow space in the porous medium and hence both velocities increase (K =  is free
flow).
The non-dimensional temperature  for different values of S and Pr is shown in figure 5. From this
figure it is concluded that an increase in Pr and S temperature decreases for both the basic fluids air (Pr = 0.71)
and water (Pr = 7.0). It is interesting to note that temperature is always move for air (Pr = 0.71) as compared to
water (Pr = 7.0) for every value of S. Moreover, for both the fluids temperature is move when heat is
observed by the fluid (- S).
The concentration profile  is shown in Figure 6 against z for different values of A, Pr and Sc. It is
concluded that increase in Pr and Sc decreases concentration but for diffusion parameter A phenomena is
opposite in nature.
Primary and secondary skin friction p and s plotted against S are shown in figures 7 and 8 for
different values of h, Gr. Gm, Pr, K and Sc. It is noted that the primary skin friction at the plate decreases with
the increase in h, Pr and Sc but increases with increase in K, Gr and Gm.
For secondary skin friction at the plate, it is observed that it increases with the increase in Gr, Gm, K
while decreases with the increase in Sc, h and Pr. Nusselt number (Nu) is shown in Figure 9, plotted against S
for the same fixed values of , n
And t. From the figure we observe that increase in Pr decreases the Nusselt number hence Nusselt
number is more for air than water.
83Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 83 | Page
REFERENCES
[1]. V. M. Soundalgekar, N. V.Vighnesam and I. Pop, Combined free and forced convection flow past a vertical porous plate, Int. J.
Energy Research 5, 1981, 215-226.
[2]. A. Raptis and C. Predikis, Mass transfer and free convection flow through a porous medium, Int. J. Energy Research, 11 1987, 423-
428.
[3]. A. S. Mohammad, Free and forced convection boundary layer flow through a porous medium with large suction”, Int. J. Energy
Research, 17 (1993), 1-7.
[4]. K. A. Helmy, MHD unsteady free convection flow past a vertical porous plate, ZAMM, J. applied mathematics and mechanics, 78
1998, 255-270.
[5]. N. C. Jain and P.Gupta, Hall effects on unsteady free convection slip flow in a rotating fluid along a porous vertical surface bounded
by porous medium, Int. J. Applied Mechanics and Engineering, 12 2007, 609-627.
[6]. B. C. Chandrasekhara and P.M.S. Namboodiri, Influence of variable permeability on combined free and forced convection about
inclined surface in porous, Int. J. Heat mass transfer, 28 1985, 199-206.
[7]. Y. Joshi and B. Gebhart, Mixed convection in porous medium adjacent to a vertical uniform heat flux surface, Int. J. Heat mass
transfer, 28 1985, 1783-1786.
[8]. F. C.Lai and F.A. Kulacki, The effect of variable viscosity on convective heat transfer along a vertical surface in a saturated porous
medium, Int. J. Heat mass transfer, 33, 1990, 1028-1031.
[9]. A. Raptis and N.G. Kafousias, N.G., “Free convection and mass transfer flow through a porous medium under the action of
magnetic field”, Rev. Roun. Sci. Tech. Mec. Appl. 27 (1982), 37-43.
[10]. A. Bejan and K.R. Khair, Effect of thermal diffusion on an oscillatory MHD convective flow with mass transfer through a porous
medium. Int. J. Heat mass transfer, 28 1985, 902-918.
[11]. E. M. A. Elbashbeshy, Heat and mass transfer along a vertical plate in presence of a magnetic field, Ind. J. Pure. Appl. Math., 27
1996, 621-631.
[12]. M. Acharya, G.C. Dash and L.P. Singh, Magnetic field effects on the free convection and mass transfer flow through porous
medium with constant suction and constant heat flux, Ind. J. Pure. Appl. Math., 31 2000, 1-18.
[13]. B. Chand, A. Kumar and V.P. Kaushik, Magnetic field effects on the free convection and mass transfer flow through porous
medium with time dependent suction and constant heat flux, Bull. Cal. Math. Soc. 95 2003, 259-272.
[14]. H. S. Tsien, Superaerodynamics mechanics of rarefied gas, J. Aeronautical Sciences, 13 1946, 653-664.
[15]. R. E. Street, A study of boundary conditions in slip flow aerodynamics in rarefied gas dynamics, Pergamon Press 1960.
[16]. S. Jothimani, and Devi, Anjali, S.P., MHD Couette flow with heat transfer and slip flow effects in an inclined channel, Ind. J. Math.
43 2001, 47-62.
[17]. N. C. Jain, B. Sharma and D. Vijay, Three-dimensional free convection heat transfer flow with periodic permeability and periodic
temperature in slip flow regime, J. Energy. Heat and mass transfer, 28, 2006, 29-44.
[18]. P. Gupta, B. Sharma and N. C. Jain, MHD heat and mass transfer slip flow in a vertical porous channel with variable suction and
heat source, Mod. Mes. Control B (Modelling, Measurement and Control B), 78 2009, 34-46.
84Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 84 | Page
85Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 85 | Page
86Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 86 | Page
87Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A
www.iosrjournals.org 87 | Page

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Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A Porous Plate With Constant Heat And Mass Flux In A Rotating System Under Slip Boundary Condition

  • 1. IOSR Journal of Mathematics (IOSR-JM) e-ISSN: 2278-5728,p-ISSN: 2319-765X, Volume 7, Issue 2 (Jul. - Aug. 2013), PP 76-87 www.iosrjournals.org www.iosrjournals.org 76 | Page Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A Porous Plate With Constant Heat And Mass Flux In A Rotating System Under Slip Boundary Condition Hoshiyar Singh1 , N.C. Jain2 and D. Chaudhary3 1 Department of Mathematics, Jaipur National University Jagatpura, Jaipur-302025, Rajasthan (India) 2 Department of Mathematics, University of Rajasthan, Jaipur-302055, Rajasthan (India) Abstract: The present analysis is made to investigate the effects of heat source and thermal diffusion on an unsteady free convection flow along a porous vertical plate in a rotating system. The plate is subjected to constant heat and mass flux also. The problem is solved analytically and expressions for velocity. Energy and temperature profiles, skin friction and Nusselt number are obtained. The effects of different parameter entered in the problem are discussed on the primary and secondary velocities, temperature and concentration distributions, primary and secondary skin frictions and Nusselt number with the help of tables and graphs. Key Words: Diffusion, Heat Source, Porous Medium, Slip Velocity, Unsteady Flow. I. Introduction The flow through a porous medium is a common occurrence in industrial environment and so the heat transfer problems of viscous incompressible fluid through a porous medium has attracted the interest of many research workers in view of its applications in geophysics, astrophysics, aerodynamics, boundary layer control and so on. A number of authors such as Soundalgekar et al. [1], Raptis and Perdikis [2], Mohammad [3], Helmy [4] and recently Jain and Gupta [5] have investigated flow through porous medium on different geometries. The effect of variable permeability on combined free and forced convection in porous media was studied by Chandrasekhara and Namboodiri [6] and Mixed Convection in porous media with uniform heat flux on vertical surface was studied by Joshi and Gebhart [7]. Lai and Kulacki [8] studied the effect of variable viscosity along a vertical surface in a saturated porous medium. The phenomena of heat and mass transfer is encountered in chemical process industries such as food processing and polymer products. Raptis and Kafousias [9], Bejan and Khair [10], Elbashbeshy [11], Acharya et al. [12], Chand et al. [13] are some of the workers to study the different problems through porous medium with mass transfer effects. In high attitude flights, situation may arise when the flow becomes unsteady and slip at the boundary take place as well. In such situation of slip flow ordinary continuum approach fails to yield satisfactory result [Tsien [14], Street [15]]. Many authors have solved problems taking slip conditions at the boundary. Recently Jothimani and Anjali Devi [16], Jain et al. [17] and Gupta et al. [18] have considered slip boundary conditions in their problems. In the present work we study the effects of heat source and permeability on unsteady free convection rotating flow of a viscous fluid past a porous vertical plate with time dependent suction and velocity slip boundary conditions. At the plate there is constant heat flux and mass flux. Perturbation technique is used to obtain the expressions of velocity and temperature fields, concentration profile, skin friction and Nusselt number. Effects of different parameters viz. Grashoff number of heat transfer, Grashoff number for mass transfer, slip parameter, permeability parameter, heat source parameter, Diffusion parameter and Schmidt number are discussed and shown graphically. It is observed that increase in Schmidt number decreases primary skin friction (p) as well as secondary skin friction (s) while increase in Grashoff number increase both the skin fictions. Moreover, increase in Prandtl number decreases Nusselt Number (Nu). II. Mathematical Formulation We consider an unsteady free convection flow of an incompressible viscous fluid through a porous medium past an infinite vertical porous plate with constant heat and mass fluxes. Let both the fluid and plate be in a state of rigid rotation with uniform angular velocity  about z-axis taken normal to the plane and plate is taken electrically non-conducting. Moreover the plate is assumed to coincide with the plane z = 0. As the plate is infinite in extent and the flow is unsteady, all the physical variables depend on z and t only.
  • 2. 77Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A www.iosrjournals.org 77 | Page For the governing equations for a free convective flow with heat source along a porous vertical plate in rotating system are given as: Continuity equation 0 z w    …(2.1) Momentum equations u K C(C'gTTg z u v2 z u w t u 2 2            …(2.2) v Kz v u2 z v w t v 2 2           …(2.3) Energy equation               TT C S z T Cz T w t T p * 2 2 p …(2.4) Concentration equation 2 2 2 2 z T D z C D z C w t C             …(2.5) Here  is the density, g is the acceleration due to gravity,  is the coefficient of volume expansion, '  is the coefficient of concentration expansion,  is the kinematic viscosity, T is the temperature of the fluid in the free stream, C is the concentration at infinite, u and v are the velocities in x and y direction respectively, T is the temperature of the fluid, K is the permeability of porous medium,  is the thermal conductivity, D is the concentration diffusivity, Cp is the specific heat at constant pressure, S* is the coefficient of heat source, Dℓ is coefficient of diffusivity. The boundary conditions are:                       zasCCTT0,v0,u 0zat D m' z Cq' z T z v Lv z u Lu …(2.6) Here q' and m' are uniform heat and concentration flux at the plate respectively, L being Mean free path. Integration of equation (2.1) gives:  nt 0 e1ww …(2.7) Using equation (2.7) and introducing following non-dimensional quantities    tw t, w n n, wz z, w v v, w u u 2 0* 2 0 *0* 0 * 0 *  2 2 0*00 K w K m' DwCC q' wTT          (Permeability parameter)    p C Pr (Prandtl number), D Sc   (Schimdt number) 2 0 w E   (Rotation velocity parameter), 2 0 2 * w S S    (Heat Source parameter)
  • 3. 78Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A www.iosrjournals.org 78 | Page    4 0 2 w q'g Gr (Grashoff number for heat transfer), Dw m''g Gm 4 0 2   (Grashoff number for mass transfer) m' Dq' A    (Diffusion parameter),   0 wL h (slip parameter) …(2.8) Equations (2.2) to (2.5) reduce to the following form after dropping the asterisks over them:                 GmGr K 1 s t q z q e1 z q nt 2 2 …(2.9)           S t Pr z e(1Pr z nt 2 2 …(2.10) t Sc z e(1Sc z nt 2 2          2 2 z A    …(2.11) where q = u +iv and s = 2iE. The corresponding boundary conditions become:                zas000,q 0zat1 z 1 zz q hq …(2.12) III. Solution Of The Problem To solve equations (2.9) to (2.11), we follow the perturbation technique in the form ( < < 1)   2 2 nt 1 0(z)qez)qq …(3.1)   2 2 nt 1 (0z)ez) …(3.2)   3 2 nt 1 0(z)ez) …(3.3) Substitution of Equations (3.1) to (3.3) in Equations (2.9) to (2.11) and equating the coefficient of like powers of  (neglecting 2 etc.), we obtain the following set of differential equations 111 1 2 1 2 GmGrq k 1 s dz dq dz qd        …(3.4) dz dq GmGrq K 1 sn dz dq dz qd 1 212 1 2 2 2        …(3.5) 1 1 2 1 2 S dz d Pr dz d     …(3.6) dz d PrS)Prn dz d Pr dz d 1 2 2 2 2 2      …(3.7)
  • 4. 79Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A www.iosrjournals.org 79 | Page 0 dz d A dz d Sc dz d 2 1 2 1 2 1 2       …(3.8) 2 2 2 1 2 2 2 2 2 dz d A dz d ScScn dz d Sc dz d        …(3.9) the corresponding boundary conditions are:                zas00000q0q 0zat0 dz d 1 dz d 0 dz d 1 dz d dz dq hq dz dq hq 212121 21212 2 1 1 …(3.10) On solving equations (3.4) to (3.9) under the transformed boundary conditions (3.10), we get the solution for ,  and q as follows   z2D 2 z1D 1 ntz1D 1 eReRee D 1 …(3.11)   z3D 8 z2D 7 z1D 6 zSc 5 ntz1D 4 zSc 3 eReReReReeReR …(3.12) z3D 19 z2D 18 z1D 17 ntz4D 11 zSc 10 z1D 9 eReReReeReReRq     z5D 22 zSc 21 z4D 20 eReReR …(3.13) Using q = u+iv, the expressions for the primary and secondary velocities are obtained as follows z1A 2 nt 20102 nt 199 ez}AsineK(KzAcoseK(K{[t)u(z,   z1Dnt 131 z3Ant 426425 eeKKeez)sinAKzAcosK     zScnt 213 z3Dnt 17 z2Dnt 15 eeKKeeKeeK …(3.14) z1A 2 nt 1992 nt 2010 ez}AsineKKzAcoseK[{(Kt)v(z,   z1Dnt 142 z3Ant 426425 eeKKeez)AcosKzAsinK     zScnt 224 z3Dnt 18 z2Dnt 16 eeKKeeKeeK …(3.15) IV. Skin Friction And Heat Transfer Once the expressions for velocities and temperature are known it is important to calculate the skin- friction and Nusselt number. The skin friction p is due to primary velocity u and skin friction s is due to secondary velocity v in the x and y directions respectively. The coefficient of skin friction in x and y directions are:            2 nt 20101 nt 199 0z x AekkAekk z u   311 nt 21173152131426325 kSckDekSckDkDkDAkAk …(4.1)            2 nt 1991 nt 2010 0z y AekkAekk z v
  • 5. 80Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A www.iosrjournals.org 80 | Page   421 nt 22183162141425326 kSckDekSckDkDkDAkAk …(4.2) and the rate of heat transfer is given by nt 211 1 eRRD1 D t)0, 1 Nu      …(4.3) where 2 b' A 2 a'1 A 2 b A 2 a1 A 4321      21 121221 2 K4164E4K{(1 a           21 121221 2 K4164E4K{(1 b           21 121221 2 4nK4164E4n4K{(1 a'           21 121221 2 4nK4164E4n4K{(1 b'              2 4SPrPr D 2 1    2 S)Pr4(nPrPr D 2 2    2 Sc4nScSc D 2 3     2 2iE)K411 D 1 4 2 2iE)nK411 D 1 5       S)PrnDPrD Pr R 1 2 1 1 2 11 2 D DR R  ,     Sc)(DSc ScA)1D R 1 1 3    ScD A R 1 4  n ScR R 3 5     nScScDD DRAScDR R 1 2 1 2 1114 6    ScnDScD DAR R 2 2 2 2 22 7    3 27165 8 D DRDRScR R  109114310219 iKKRKiKRiKKR  81472136512 RGmRRGmRGrRiKKR
  • 6. 81Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A www.iosrjournals.org 81 | Page  1615181413178716121115 iKKRiKKRiKKRiKKR  262522222121201920181719 iKKRKiKRiKKRiKKR       221 1 2 1 2 1 1 1 2 141 1 4EKDDD KDDRGmDGr K      221 1 2 1 2 1 41 2 4EKDDD RGmD(Gr2E K       2212 3 12 3 4EKScSc RGmKScSc K     2212 3 4 4EKScSc RGm2E K  11515 DKRGmRGrK  126 DKK  357 KScRGmK  48 KScK            2 2 22 1 41223111 9 AhAh(1 Sc)]h1KhD1KAhSc)]h1KDh1KAh1 K ,            2 2 22 1 31124121 10 AhAh(1 Sc)h1KDh1KAhSc)]h1KDh1KAh1 K ,  1029111 KARAK  1019212 KARAK              221 1 2 1 6 1 1 2 15 13 4EKnDD K2EnDDK K ,               221 1 2 1 5 1 1 2 16 14 4EKnD(D K2EKnDDK K       221 2 2 2 1 2 2 213 15 4EKnDD KnDDR K     221 2 2 2 13 16 4EKnD(D R2E K       221 3 2 3 1 3 2 314 17 4EKnDD KnDDR K     221 3 2 3 14 18 4EKnD(D R2E K              2 221 21 1 2 2 2 1 22112 1 1 2 2 2 111 19 2E)AA2AKnAA(A 2E)AA2AKKnAAAK K ,              2 221 21 1 2 2 2 1 22111 1 1 2 2 2 112 20 2E)AA2AKnAA(A 2E)AA2AKKnAAAK K ,
  • 7. 82Effects Of Heat Source And Thermal Diffusion On An Unsteady Free Convection Flow Along A www.iosrjournals.org 82 | Page              212 8 12 7 21 4EKnSc(Sc K2EKnScScK K ,              2212 7 12 8 22 4EKnSc(Sc 2EKKnScScK K , hSc)],1KhAK hA1KhD1KhD1KhD1KK 21220 11931721511323   hSc)],1KhAK hA1KhD1KhD1KhD1KK 22219 12031821611424               2 4 22 3 424323 25 AhhA1 hAKhA1K K             2 4 22 3 423324 26 AhhA1 hAKhA1K K V. Discussion And Conclusions In order to get physical insight of the problem, calculations have been made for primary and secondary velocities (u,v), temperature (), concentration (), primary and secondary skin-frictions (p,s) and Nusselt number (Nu) for different parameters viz. Prandtl number (Pr), Schmidt Number (Sc), Permeability parameter (K). Heat source parameter (S), Grashof number for heat transfer (Gr), Grashof number for mass transfer (Gm), Diffusion parameter (A) and Slip parameter (h) fixing  = 0.02, E = 0.4, n = 0.1 and t = 1.0. From Figure 1, important observation is that increase in h, increases the primary velocity near the plate but after some distance it decreases Physically it due to the fact that effect of slip parameter nullify as we go far from the plate. However, in case of Gm and S velocity increases as both the parameters decreases but Gr has opposite phenomena. From Figure 2, for secondary velocity v (in the figure we have plotted – v ) the observations are same as that of primary velocity for the case of Gr, Gm and S but interestingly as h increases secondary velocity decrease near the plate but goes on increasing as we move away from the plate. In figure 3 and 4 the primary and secondary velocities u and v are plotted for different values of Pr, K and Sc. From the figures we observed that an increase in Pr and Sc decreases primary but increases secondary velocity. It is further observed that for increasing K both velocities (u,v) increases. Physically, we say that increase in K increases the flow space in the porous medium and hence both velocities increase (K =  is free flow). The non-dimensional temperature  for different values of S and Pr is shown in figure 5. From this figure it is concluded that an increase in Pr and S temperature decreases for both the basic fluids air (Pr = 0.71) and water (Pr = 7.0). It is interesting to note that temperature is always move for air (Pr = 0.71) as compared to water (Pr = 7.0) for every value of S. Moreover, for both the fluids temperature is move when heat is observed by the fluid (- S). The concentration profile  is shown in Figure 6 against z for different values of A, Pr and Sc. It is concluded that increase in Pr and Sc decreases concentration but for diffusion parameter A phenomena is opposite in nature. Primary and secondary skin friction p and s plotted against S are shown in figures 7 and 8 for different values of h, Gr. Gm, Pr, K and Sc. It is noted that the primary skin friction at the plate decreases with the increase in h, Pr and Sc but increases with increase in K, Gr and Gm. For secondary skin friction at the plate, it is observed that it increases with the increase in Gr, Gm, K while decreases with the increase in Sc, h and Pr. Nusselt number (Nu) is shown in Figure 9, plotted against S for the same fixed values of , n And t. From the figure we observe that increase in Pr decreases the Nusselt number hence Nusselt number is more for air than water.
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