In viscoelastic media, the slowness vector **p** of plane waves
is complex-valued, **p**=**P**+i**A**. The
real-valued vectors **P** and **A** are usually called the
propagation and the attenuation vector, respectively. For **P**
and **A** nonparallel, the plane wave is called inhomogeneous.

Three basic approaches to the determination of the slowness vector
of an inhomogeneous plane wave propagating in a homogeneous
viscoelastic anisotropic medium are discussed. They differ in the
specification of the mathematical form of the slowness vector
**p**. We speak of directional specification, projection
specification and mixed specification of the slowness vector.
Individual specifications lead to the eigenvalue problems for
3 x 3 or 6 x 6 complex-valued matrices.

In the directional specification of the slowness vector, the
real-valued unit vectors **N** and **M** in the direction of
**P** and **A** are assumed to be known. This has been the
most common specification of the slowness vector used in the
seismological literature. In the componental specification, the
real-valued unit vectors **N** and **M** are not known in
advance. Instead, the complex-valued vectorial component
**p*** ^{Sigma}* of slowness vector

The simplest, most straightforward and transparent algorithms to determine the phase velocities and slowness vectors of inhomogeneous plane waves propagating in viscoelastic anisotropic media are obtained, if the mixed specification of the slowness vector is used. These algorithms are based on the solution of an algebraic equation of the sixth order. Alternatively, they are based on the solution of a conventional eigenvalue problem for 6 x 6 complex-valued matrices. The derived equations are quite general and universal. They can be used both for homogeneous and inhomogeneous plane waves, propagating in elastic or viscoelastic, isotropic or anisotropic media. Contrary to the mixed specification, the directional specification can hardly be used to determine the slowness vector of inhomogeneous plane waves propagating in viscoelastic anisotropic media. Although the procedure is based on 3 x 3 complex-valued matrices, it yields a cumbersome system of two coupled equations.

Viscoelastic anisotropic media, inhomogeneous plane waves, phase velocity, slowness vector.

The image of the paper in GIF 150dpi (1 000 kB!) is designed for an instant screen preview.

The paper is available in PostScript (233 kB) and GZIPped PostScript (86 kB).

In: Seismic Waves in Complex 3-D Structures, Report 13, pp. 169-187, Dep. Geophys., Charles Univ., Prague, 2003.

SW3D - main page of consortium