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The intensity of the fictitious discontinuity source depends on both the mean wave field and the irregularities.
The phase velocities and attenuation factors of the mean wave field in the composites are analyzed for various elastic properties, density and volume concentrations of the inclusions.
The dispersion equations for the wave numbers of the mean wave field in such composites are derived using two different versions of the EMM.
One is a mean wave field, which is response field in a perfectly layered half-space subjected to a seismic dislocation source.
The mean wave field is associated with a buried seismic dislocation source, while the scattered wave field is associated with a set of fictitious discontinuity sources distributed on the fictitious mean interface, which has the same effect as the interface irregularities and can be obtained in terms of the mean wave field.
The effective field method (EFM) and quasi-crystalline approximation are used for the calculation of phase velocity and attenuation factor of the mean wave field propagating through the composite.
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Velocities and attenuation factors of the mean wave fields in the composites obtained by different versions of the EMM are compared for various volume concentrations and properties of the inclusions.
This doesn't mean waving Bibles.
The restaurant's name means "wave" in Greek.
He meant "waving the Saltire".
An analytical solution of these equations is presented for uniform ducts carrying an incompressible mean flow and the wave field is shown to consist of superposed forward and backward acoustic waves and a hydrodynamic wave, which occur in general as coupled waves.
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Justyna Jupowicz-Kozak
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