2. Analytical Solution 523
Equations IIIa.3.20-1 and IIIa.3.23-1 are second-order, coupled partial differen-
tial equations. Finding an analytical solution by integration is not an easy task.
However, in this case we know how the profiles of both variables look like.
Therefore, we try to solve these equations by guessing the functional relationship
for V
x
= f
1
(y) and T = f
2
(y). Since for each equation we have four boundary condi-
tions, two at the surface and two at the edge of boundary layer, we use a third or-
der polynomials. Thus, we express velocity as a function of y as:
3
4
2
321
ycycyccV
x
+++=
All we have to do now is to find the four unknown coefficients, c
1
through c
4
, so
that the above polynomial fits both Equation IIIa.3.20-1 and the specified sets of
boundary conditions. The sets of boundary conditions are:
at y = 0: V
x
= 0 and ∂
2
V
x
/∂y
2
= 0
at y =
δ: V
x
= V
f
and ∂V
x
/∂y = 0
Using conditions at y = 0, we find c
1
= c
3
= 0. We now use conditions at y = δ to
find c
2
and c
4
. From y = δ, V
x
= V
f
, we find c
2
δ + c
4
δ
3
= V
f
. From y = δ, ∂V
x
/∂y =
0, we find c
2
+ 3c
4
δ
2
= 0. Solving this set, we find c
2
and c
4
in terms of δ, V
x
, and
V
f
as c
2
= 3V
f
/2δ and c
4
= –V
x
/2δ
3
. Therefore, the velocity profile becomes:
3
į2
1
į2
3
¸
¹
·
¨
©
§
−=
yy
V
V
f
x
IVb.2.1
Due to the similarity of the governing Equations IIIa.3.20-1 and IIIa.3.23-1, we
expect that temperature can be described by a similar function:
3
į'2
1
į'2
3
¸
¹
·
¨
©
§
−=
−
−
yy
TT
TT
sf
s
IVb.2.2
Although we were able to find an analytical solution for these profiles, we are far
from declaring victory. This is because in Equation IVb.2.1, V
x
is expressed in
terms of the unknown
δ, yet to be determined. We did expect this additional twist,
as we used our engineering intuition and picked a profile. We then found the co-
efficients of the function representing the profile from the boundary conditions.
But we still have no guarantee that the chosen profile would satisfy the governing
equation itself. The thickness of the boundary layer,
δ, is indeed the final re-
quirement to ensure the chosen profile does satisfy the governing equation. We
should then embark on finding
δ. Similar to the profile for V
x
, we first guess a
profile for
δ and then try to find the related coefficient. However, the solution for
δ is not as straightforward as the solution we managed to find for the velocity pro-
file.