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FREE CONVECTION BOUNDARY LAYER FLOWOF A MICROPOLAR FLUID PAST SLENDER CONES H.S. Takhar Simon Engineering Laboratories, University of Manchester, Manchester, England M139PL. Rama Subba Reddy Gorla, Professor and Chairman Department of Mechanical Engineering, Cleveland State University Cleveland, Ohio 44115 William R. Schoren, Research Assistant Department of Mechanical Engineering, Cleveland State University, Cleveland, Ohio 44115 (Received 16 April 1987; accepted for print 5 April 1988)
Abstract Using the theory of micropolar fluids developed by Eringen, the transverse curvature effects on axisymmetric free convection boundary layer flow of a miropolar fluid past slender vertical cones are investigated. The case of constant surface heat flux is considered in this paper. Using perturbation techniques, the governing equations for momentum, angular momentum and energy have been solved numerically. Graphical representations for the velocity, angular velocity and thermal functions are presented for various physical and fluid property parameters. Introduction Free convection flow is caused by buoyancy forces which arise from density differences in a fluid. These density differences are a consequence of temperature gradients within the fluid. Free convection flow is a significant factor in several practical applications which include, for example, chemical processes and related equipment and the cooling of rotating machinery and electronic components. Eringen [ i ] has developed the theory of micropolar fluids and has extended this theory to include thermomicropolar fluids [2]. A comprehensive review of research involving micropolar fluid mechanics was provided by Ariman, et. al. [3,4]. The laminar free convection boundary layer flow of a thermomicropolar fluid past a non-isothermal vertical flat plate was 167
168
H.S.
TAKHAR,
R.S.R.
GORLA
a n d W.R.
SCHOREN
i n v e s t i g a t e d by Jena and Mathur [ 5 ] . They derived a s i m i l a r i t y s o l u t i o n by p r e s c r i b i n g the plate temperature as a l i n e a r function of the streamwise coordinate. The present work has been undertaken in order to study the influence of transvere curvature on laminar free convective boundary layer flow of a thermomicropolar f l u i d past a slender v e r t i c a l cone. The case of a constant surface heat f l u x from the cone is i n v e s t i g a t e d in t h i s paper.
G0verningE_q_u_ationA In the analysis that f o l l o w s ,
three general assumptions are made: ( I )
temperature of the cone everywhere exceeds that of the ambient f l u i d . The cone angle '@' has a constant p o s i t i v e value less than 45 ° . fluid
(3)
The
(2) All
properties are constant except those causing the buoyancy e f f e c t . Although the reverse case for the f i r s t
mathematically
identical,
assumption can be shown to be
the consequence of the f i r s t
free convection flow is in the upward d i r e c t i o n (x = O) w i l l
be pointed downward.
(Figure I ) .
assumptions allows the use of the f o l l o w i n g equations for an incompressible,
assumption is that the
and the vertex of the cone The second and t h i r d
partial
differential
axisymmetric, steady, laminar free
convection boundary layer flow of a micropolar f l u i d : Mass : ~_ (ru) + ~__ ( r v ) = 0 Bx ~)r
(I)
Momentum : uDU + D x va~U =~r
E v + Kp_--I --Ir T r
--rDU] + < IN + ~T~] + GB(T-T )cos$ _ ~i
~
(2) Angular Momentum: u DN + v aN = ~ a-xDr pj
{L ~_[--rDN~ - N } _ ~ _ {Du + 2N} r BrL_ a r ] ~ PJ ~-r
(3)
Energy: uaT + vaT = ~11 a l--raT-] ax D--ff r a--r-I_ ~rl J
The use of these governing equations l i m i t s the a p p l i c a t i o n of t h i s analysis to slender cones because these equations do not account for the
(4)
M I C R O P O L A R B O U N D A R Y L A Y E R PAST C O N E S
buoyancy e f f e c t s in the ' r '
or radial d i r e c t i o n .
169
The boundary conditions for
the v e l o c i t y f i e l d are: At r = xtan¢:
u = v = O,
L~r_1
2 As r ÷ -:
(5)
N : _1 BF-I A-l
u + O, N +0
The boundary conditions for the temperature f i e l d are: At r = x t a n ¢ : As r + -:
(6)
T = Tw = T® + H 3(m h ( x )
T + T~
Analysis In solving the continuity equation or the equation of the conservation of mass, a stream function ¢ ( x , r ) is usually defined such t h a t : 1~,i, u
:
= ~
r @r
;
v
:
(7) r @x
In order to f a c i l i t a t e the solution of the other governing equations, the following coordinate transformation are defined: : 2 ~ x Ctan¢
_[m+3l -4--
; n : r2 - x2 tan2¢ {x 2 tan2¢
where 1/4 : x ;
L ¢(xr)
C : [-GSHL3c°s¢l-~ L_ u2 ]
: vLC t a n ¢ ~
m+7 4 f({n)
[m+l] N = 2v2C2 P ~ T g ( { n ) r{[ h(x)
: e({,n)
: T-T=
HR'"
170
H.S.
= ~ ;
TAKHAR,
X =
Substituting
~ uj
R.S.R.
;
GORLA
and
W.R.
SCHOREN
B = x2tan2¢ J
the expressions
(8)
in (7) and (8) i n t o
equations
(2)-(4)
yields
the f o l l o w i n g :
+ e = ~F-m+3~
I-4 I_
4~(I+~n)2 g,,
._
-
2
_
~f-" a~f- f
I_
a__~f'_-}
(9)
]
A2B(I+~n)2 ~2 f,, _ 2B(l+~n)~2g
-
.~
~n + (3m + 5-_ f ' g + ( l + ~ n ) ( m + 7 ) f g '
(I0)
-
_ --2-
~__--oaf- f' ~_0_ (ii)
A prime denotes d i f f e r e n t i a t i o n
with
equations.
The boundary c o n d i t i o n s
coordinates
are:
f(~,O)
= f'(~,O)
= O;
g(~,O)
= -~f"(~,O); 2
f'(&,-)
r e s p e c t to
'n'
f o r the v e l o c i t y
o n l y in the above field
in the t r a n s f o r m e d
= 0
(12)
The boundary c o n d i t i o n s
g(~,-)
= 0
f o r the t e m p e r a t u r e
in the t r a n s f o r m e d
coordinates
are: 0(~,0)
The f o l l o w i n g
= h(x)
= 1 + ~ anon; n=O
@(~,~) = 0
power s e r i e s expansions are assumed f o r the v e l o c i t y ,
(13)
angular
MICROPOLAR
BOUNDARY
LAYER PAST CONES
v e l o c i t y and thermal functions in order to solve the p a r t i a l equations (9),
171
differential
(I0) and ( I I ) : : f0(n) + ~ f l ( n )
+ ~2f2(n) + . . . .
(14)
g(C,n) : go(n) + { g l ( n )
+ {2g2(n) + . . . .
(15)
e(C,n) : e0(n ) + Cel(n) + C2B2(n) + . . . .
(16)
f(~,n)
Substituting (14), (15) and (16) into equations (9), (10) and ( I i ) and equating equal powers of { to zero yields a set of ordinary differential equations governing the momentum, angular momentum and energy fields.
These
details are not shown in the interest of conserving space. Although various wall temperatures are allowed by equation (13), the case of constant wall heat f l u x w i l l local
be considered here.
Using Fourier's Law, the
heat t r a n s f e r rate from the cone surface i s :
qw
: -kl -G~H5 cos¢_ I / 4 ~ [5m-l] T(@e) L
(17)
" :o
In order for the heat f l u x from the cone surface 'qw' to be maintained constant, the following conditions must hold t r u e : m:0.2 e'(0) : 0 for n > 0 n Therefore :
1/4
L T]
qw : -kF-GBH5 COS¢--I
06(0)
(18)
Since 'qw' is constant, an expression for 'H' can be found from equation (18) and s u b s t i t u t e d i n t o the expression for e(~,n) from equation (8).
Rearranging
t h i s expression and noting that T = Tw at the wall y i e l d s an equation for the wall temperature: T : T = T +~- v2qw~ w l k4GBcoso
-B~ (
Z en(O){ n n=0
(19)
172
H.S.
TAKHAR,
R.S.R.
GORLA
and W.R.
SCHOREN
Applying the conditions for constant surface flux yields the following equations: 0.4 [ ( i + _A) f" Cf x = 2C3 -#
NUx
=
(20)
-HCx %(O) (Tw_T)
Nux : -[h(x)] Grx-~
-5/4
(21)
O' 0(0)
Numerical solutions to equations governing f j ( n ) ,
(22)
gj(n) and ej(n) have been
found using A, ~, B and Pr as parameters. A step size for n of 0.001 was used along with double precision arithmetic for all computations. Shooting techniques were used to determine unknown values for the v e l o c i t y , velocity,
angular
and thermal functions at the cone surface.
From Figure 2, i t can be observed that the second term of the power series expansion for the velocity function, namely f ' has negative values. We note that the f i r s t term f '
represents the velocity function when
transverse curvature effects are ignored.
This implies that the velocity of
the convective f l u i d decreases as the transverse curvature increases.
This
conclusion is in concurrence with the previous statement since smaller temperature gradients give rise to smaller f l u i d velocities.
In free
convection flow, the driving force for fluid motion is density differences due to fluid temperature gradients.
Therefore the f l u i d velocity will decrease as
the temperature gradient in the f l u i d decreases with increasing transverse curvature.
Figures 3 and 4 represent numerical solutions for the angular
velocity and thermal functions respectively.
Concluding Remarks In this paper, the theory of thermomicropolar fluids formulated by Eringen has been used to derive a set of boundary layer equations for axisymmetric free convective flow past slender vertical cones. The case of constant surface heat flux has been considered.
Perturbation techniques have
MICROPOLAR
BOUNDARY
LAYER
PAST C O N E S
173
been used to generate numerical solutions for the governing equations for momentum, angular momentum, and energy. Graphical representations for the velocity, angular velocity, and thermal functions are presented for various dimensionless material properties of the micropolar fluid. surface friction factor and Nusselt number are given.
Equations for the
The numerical results
obtained have clearly demonstrated that the surface temperature of the cone increases less rapidly in the streamwise direction with increasing transverse curvature.
I t also has been shown that the fluid velocity decreases with
increasing transverse curvature. Nomenclature a
coefficient for the surface temperature function
B
dimensionless physical parameter
C
dimensionless constant
Cfx
local friction coefficient
f(¢,n)
-
dimensionless velocity function
g(~,n)
-
dimensionless microrotation function
G
acceleration due to gravity
Grx
local Grashof number
h(x)
surface temperature function
H
temperature constant
J
micro-inertia per unit mass
k
thermal conductivity
K
microrotation viscosity parameter
L
reference length
m
exponent for the surface temperature
N
angular velocity
Nu
Nusselt number
Pr
Prandtl number
q
heat flux
r
radial coordinate
Re
Reynolds number
T
temperature
U
velocity in the x-direction velocity in the y-direction
V
174
H.S.
x
TAKHAR,
R.S.R.
GORLA
and W.R.
-
d i s t a n c e along the cone surface
x
-
dimensionless v a r i a b l e
y
-
c o o r d i n a t e in the r a d i a l
~,n
-
dimensionless coordinates
~,~
-
dimensionless f l u i d
-
coefficient
-
dynamic v i s c o s i t y
-
kinematic v i s c o s i t y
p
-
d e n s i t y of f l u i d
¥
-
material
-
thermal d i f f u s i v i t y
O(C,n)
-
dimensionless temperature f u n c t i o n
-
conditions
-
ambient c o n d i t i o n s
SCHOREN
in the x - d i r e c t i o n direction
properties
of thermal expansion
p r o p e r t y of the f l u i d
Subscripts w
at the cone surface
References [1]
A.C. Eringen, "Theory of M i c r o p o l a r F l u i d s " ,
Journal of Mathematics and
Mechanics, 16, pp. 1-18. (1966). [2]
A.C. Eringen,
"Theory of Thermomicrofluids",
Analysis and A p p l i c a t i o n s , [3]
T. Ariman, M.A. Turk and N.D. S y l v e s t e r , -
A Review", I n t e r n a t i o n a l
pp. 905-930. [4]
38, pp. 480-496.
"Microcontinuum F l u i d Mechanics
(1973).
F l u i d Mechanics", I n t e r n a t i o n a l
[5]
(1972).
Journal of Engineering Science, 11,
T. Ariman, M.A. Turk and N.D. S y l v e s t e r ,
pp. 273-293.
Journal of Mathematical
"Applications
of Microcontinuum
Journal of Engineering Science, 12,
(1974).
S.Ko Jena and M.N. Mathur, " S i m i l a r i t y
Solutions f o r Laminar Free
Convective Flow of a Thermomicropolar F l u i d Past a Non-lsothermal Vertical
Flat P l a t e " ,
International
19, pp. 1431-1439. (1981).
Journal of Engineering Science,
MICROPOLAR
BOUNDARY
LAYER
PAST C O N E S
175
G
v~<~
Figure I .
I
r
Geometrical Configuration for Flow Past Cone
0,8 Pr=lO.O0 =20.00 0.6
A =10.00
B =0.10 m =0.20
0.4
0.2
0 2
3
4
5
B
-0.2
-0.4
-0,6
-0.8
-1.0
-1.2
Figure 2.
Distribution for the Velocity Functions
176
H.S.
TAKHAR,
R.S.R.
GORLA
and W.R.
SCHOREN
0~ Pr=lO.O0 ~20~00
06
I/
A=10.00 El=0.10
%
oI
+ ~4-
-0.4 ~ /
~
-0.6 ~
- -~----.__j_~. --+====~.~>_-~
gl XlO' g~
-0.8 I
10 } i
-12 t Figure
3.
Distribution
for the Angular Velocity
\ 0.4
Functions
Pr=lO.O0 =20.00 A=10.00 m=o,2o
0+2o
-0.2 -0.4
-0.6 -0.8
-1.2
F i g u r e 4.
Distribution
f o r t h e Thermal
Functions