Boundary-Layer Flow Past a Semi-Infinite Wedge: The Falkner-Skan Problem
Boundary-Layer Flow Past a Semi-Infinite Wedge: The Falkner-Skan Problem
In 1904 Prandtl showed that the effects of viscosity at a high Reynolds number could be represented by approximating the Navier–Stokes equations with the celebrated boundary-layer equations, which for two-dimensional steady flow reduce to:
V
X
∂
V
X
∂X
V
Y
∂
V
X
∂Y
U
X
2
∂
V
X
∂
2
Y
∂
V
X
∂X
∂
V
Y
∂Y
V
X
V
Y
V
X
Here, and are the coordinates parallel and perpendicular to the body surface, respectively.
X
Y
For a semi-infinite wedge with an angle of taper , one can prove that far from the wedge the potential flow is given by
ω=βπ
U(X)=A
m
X
m=
βπ
2π-βπ
β=
2m
m+1
A
The above boundary-layer equations admit a self-similar solution such that the velocity profiles at different distances can be made congruent with suitable scale factors for and . This reduces the boundary-layer equations to one ordinary differential equation.
X
X
Y
Let us introduce a function such that: =Af'(η) where .
f(η)
V
X
m
X
η=Y
(m+1)A
2ν
m-1
2
X
Then, we have from continuity equation: =-(m+1)Aνf(η)+ηf'(η).
V
Y
1
2
m-1
2
X
m-1
m+1
The boundary-layer equations can be written as follows:
f'''(η)+f(η)f''(η)+β1-=0
2
(f'(η))
with and
f(η=0)=f'(η=0)=0
f'(η→∞)=1
The above equation can be solved for a user-set value of parameter when and using the shooting technique. The limiting case is flow over a flat plate (Blasius problem). Using the following definitions of = and =, one can obtain the particle trajectories (streamlines) for different starting points. This Demonstration plots such trajectories and also shows the growth of the boundary-layer (red curve) in a separate plot for any value of the wedge angle. The evolution of the -velocity component and its congruent properties with the growth of the boundary layer is also shown.
β
A=1
ν=1
β=0
V
X
X
t
V
Y
Y
t
δ(X)
V
X