Our point of departure for the basic theory of aeroacoustics is an exact
restatement of the continuity and momentum equation for a compressible
fluid, i.e. the Navier-Stokes equations2, to the following form:
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(1) |
The left-hand side of this equation can be recognized as the wave equation,
in this case for the acoustic pressure perturbation
which
propagates with the speed of sound
. The equation given above shows that
these propagating pressure fluctuations are due to various sources, which
are the terms on the right-hand side. The first term on the the right-hand
side denotes sound production due to unsteady mass injection and the second
term the sound produced by external forces acting on the fluid. These two
terms are known as the classical acoustic sources as for instance discussed
by Rayleigh (1945). The third term of the Lighthill equation is the
non-linear advection term, which is mainly responsible for the sound produced by
the flow. This term is in particular large in a turbulent flow3.
The fourth term represents the deviations from an
isentropic state, including effect of non-constant speed of sound,
convection and refraction of sound by temperature gradients. Basically all
the acoustic effects associated with the internal energy
of
the flow are lumped in this term. It should be noted that in the Lighthill
theory the equation for the internal energy is absent. The fifth term, in
which
denotes the strain rate tensor, is due to viscous effects. These
effects are in general very small except for the boundary-layers
close to solid walls where the strain
can become very large.
The
first two sound sources are due to externally applied processes and fall by
definition outside the scope of this research project. We will focus on the
sound generated by the flow itself and in particular on the non-linear term,
which for most practical circumstances is the most important contributor to
flow noise. This is supported by considering the ratio of the non-linear
inertial term to the viscous term given by