LAB 8 - Velocity Profile above a Flat Plate
Introduction
In any viscous flow, the fluid in direct contact with a solid boundary has
the same velocity as the boundary itself and the "no-slip condition" must
be satisfied at the boundary. Since the fluid velocity at the stationary
solid surface is zero, but the bulk fluid is moving, velocity gradients (and
hence shear stress) must be present in the flow. For one-dimensional viscous
flow, the shear stress t is given by
(1)
where
= dynamic viscosity, u = stream wise velocity,
and y = normal coordinate measured from the solid
boundary.
Thus, for external flow over a flat plate as shown in Figure 1, the wall
shear stress can be determined from knowledge of the velocity profile.
For an external flow in which the fluid is unbounded by walls, the viscous
effects will grow and continually expand as flow moves further downstream
along the solid surface. The viscous layers, either laminar or turbulent,
are very thin, much thinner than the drawing above shows. The boundary
layer thickness is defined as the point where the velocity u parallel
to the plate reaches 99% of the external free stream velocity U.
The accepted formulas offor
flat-plate flow are [1]
/x 5.0/Rex1/2 for laminar
flow (2)
In turbulent flow, the boundary layers expands more rapidly and the accepted
correlation for is
/x
0.16/Rex1/7
for turbulent flow
(3)
A dimensionless quantity of particular interest in external flows is
cf, called the skin-friction coefficient, and is analogous to
the friction factor f in internal flows. cf is defined by
cf
= 2/U2
(4)
where U = the free stream velocity outside the boundary layer,
= the shear stress
at the wall, and =
the density of the fluid.
Boundary layer theory, first formulated by Ludwig Prandtl in 1904, is one
method for obtaining solutions for laminar flow inside a boundary layer.
By making certain order of magnitude assumptions the Navier-Stokes
equations can be simplified into the boundary layer equations that may be
solved relatively easily in some simple geometries. Equation 3, Blassius's
solution is a result of a boundary layer solution. Blassius's
solution results in an ordinary differential equation that must be numerically
integrated. The tabular result is available in the fluid mechanics textbook
[1]. It also provides a solution for cf in laminar flow given
by
cf = 0.664/Rex1/2 (5)
There are three regions in the boundary layer in a turbulent flow: 1) the viscous or wall layer (viscous shear dominates), 2) outer layer (turbulent shear dominates), 3) overlap layer (both types of shear important). There is no exact theory for turbulent flat-plate flow, although there are many computer solutions of the boundary-layer equations using various empirical models. Another technique that produces a widely accepted result is an integral analysis where a logarithmic law is assumed for the velocity profile. It is convenient to introduce a a parameter u*, called the shear velocity or friction velocity, to nondimensionalize the velocity profile. This is given by
u* =
()1/2 (6)
The logarithmic law that we assume holds all the way across the boundary
layer is
(7)
where the constants = 0.41
and B = 5.0. This equation was obtained by examining boundary
layers experimentally. By applying equation (7) at the edged of the
boundary layer where
y = and u =
U, and using the definition of skin-friction coefficient in equation
(4) the following skin-friction law for turbulent flat-plate flow can be
obtained.
(8)
Experimental Apparatus
A flat plate with a length of 14 inches has been secured inside
the test section of the AERO lab wind tunnel. A pitot tube is mounted
above the test section (O.D. = 0.10 in) at a distance of approximately
12 inches from the leading edge of the plate. The pitot tube can be moved
in the y-direction above the plate using a traversing mechanism that is scaled
in 0.001" increments (1 revolution = 0.025 in). Both the static and stagnation
pressure taps on the pitot tube are connected to a manometer in order that
the difference between these two pressures may be measured directly in inches
of water. Other instrumentation includes a thermistor inserted into the flow
stream at one of the ports on the side walls of the test section. The air
velocity can be determined from the pressure difference data and the air
density. The wall shear stress and skin-friction coefficent can be calculated
from the velocity profile.
Pitot Tube
If Red > 1000, where d is the probe diameter, the
flow around the probe is nearly frictionless and Bernoulli's equation applies
with good accuracy. For incompressible flow, and neglecting any elevation
head, the following expression relates the local velocity to the difference
in stagnation and static pressure:
(9)
where po = stagnation pressure,
ps = static pressure,
and =
fluid density.
The difference between the stagnation and the static pressure can be measured
in terms of h inches of water so that equation 9 can be rewritten as
(10)
where k is a constant.
Objectives
Procedure
Data Reduction & Points of Interest
References