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Vorticity production in turbomachines and its influence upon meridional flows
sible flow problem. Although this is possible, a more direct analysis, offering also
deeper perception of the physical nature of compressible flows, follows from adoption
of the velocity potential instead of the stream function. This will be introduced in
the next section.
6.6.2 Analogy between compressible flows and incompressible flows with source
distributions
The continuity equation in vector form has already been stated as follows:
div p~ = 0 Compressible flow 1 [6.4]
div ~ = 0 Incompressible flow
J
The equation for incompressible flow may be further developed to accommodate
spatial distributions of source strength S, defined as fluid created at any point per
unit volume per unit time. Equation (6.4b) then becomes
div ~ = S (6.64)
An analogy with compressible flow follows if the vector derivative of Eqn (6.4a) is
expanded, namely
div p~ = p div ~ + ~. grad p = 0
Rearranging this, the compressible ftow continuity equation may be expressed as
1
div~ : ---~.gradp
(6.65)
P
=or
The quantity on the right-hand side,
-(1/p)~.gradp,
which absorbs all of the
compressibility effects could be treated analytically as an equivalent distributed source
density or in incompressible flow; thus Eqns (6.64) and (6.65) are identical in form.
In the one case the Poisson term S is due to distributed source strength. In the other
case the Poisson term or is caused by local gradients of fluid density.
Let us now apply this idea to the free-vortex turbine stator illustrated in Fig.
6.11(a), modelled by an actuator disc AD. In this
free-vortex
case the flow is
irrotational and there is no tangential vorticity too shed from the blade row. Instead
the fluid is assumed to undergo a sudden drop in density in the plane of the actuator
disc, or in other words a sudden rise in specific volume. As shown by Lewis and
Horlock (1969) this is physically analogous to the incompressible flow through a
source actuator disc, Fig. 6.11 (b), the streamline shifts and velocity distributions being
the same. These authors have presented a full exposition, the main outline of which
will be given here. Since too is to be zero, Eqn (6.11c) becomes
tgC r aC x
s ~ 0
ox ar