
80 APPLICATIONS IN FLUID DYNAMICS
complete analysis was done by Cochran
16
; an overview of the analysis and use
of this instrument is given by Levich.
17
This problem can be solved analytically
for laminar flow conditions in the absence of free convection effects. However,
under proper operating conditions, the hydrodynamics take on a boundary-layer
character such that the change in velocity components occurs within a thin region
of influence near the rotating disk. Establishing a thin boundary layer is important
for heat- or mass-transfer characterization using this apparatus since it ensures that
container boundary effects are minimized. We use scaling analysis to ascertain the
conditions for which the boundary layer will be thin.
A surprising aspect of laminar rotating disk flow is that there is no radial pressure
gradient and the radial and angular velocities are directly proportional to the radial
position, whereas the axial velocity depends only on the axial position. Classical
treatments of this flow begin by recognizing these considerations intuitively and
then proceeding to develop the rigorous analytical solution for this flow. However,
these considerations can be ascertained via simple integral mass and momentum
balances. Consider a mass balance on a control volume of arbitrary radius r extend-
ing from the surface of the disk far into the fluid, where there is only an axial
velocity component given by u
z
=−U
∞
. Note that in practice U
∞
is unknown;
however, it can be determined from the solution for the hydrodynamics and a
specified disk rotation rate. A mass balance on this control volume then yields
U
∞
πr
2
= 2πr
∞
0
u
r
dz ⇒ U
∞
=
2
r
∞
0
u
r
dz ⇒ u
r
= rf
1
(z) (3.E.4-1)
If the general form of the radial velocity profile given by equation (3.E.4-1) is sub-
stituted into the continuity equation given by equation (C.2-1), we can conclude
that the axial velocity is independent of r:
1
r
∂
∂r
(ru
r
)+
∂u
z
∂z
=0 ⇒ 2f
1
(z)+
∂u
z
∂z
=0 ⇒ u
z
=−2
z
0
f
1
(˜z) d ˜z =f
2
(z)
(3.E.4-2)
where ˜z denotes a dummy integration variable. Hence, we conclude that u
z
is a
function only of z. We can now prove that there is no radial pressure gradient
by considering an integral z-momentum balance on a control volume of arbitrary
radius r extending from an arbitrary height z into the fluid far from the rotating
disk where u
z
=−U
∞
:
ρU
2
∞
πr
2
−
r
0
ρu
2
z
· 2π ˜rd˜r
z
− P
∞
πr
2
+
r
0
P · 2π ˜rd˜r
z
+
∞
z
τ
rz
· 2πrd˜z
z
−
r
0
τ
zz
· 2π ˜rd˜r
z
= 0 (3.E.4-3)
16
W. G. Cochran, Proc. Cambridge Philos. Soc., 30, 365–375 (1934).
17
V. G. Levich, Physicochemical Hydrodynamics, Prentice-Hall, Englewood Cliffs, NJ 1962, pp. 60–78.