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THE SPECTRAL FUNCTION OF A VERTICALLY INHOMOGENEOUS MEDIUM1
- Source: Geophysical Prospecting, Volume 36, Issue 1, Jan 1988, p. 1 - 5
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- 27 Apr 2006
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Abstract
Elastic, acoustic and electromagnetic waves in media consisting of vertically inhomogeneous layers are considered in a common formulation. The spectral function of a vertically inhomogeneous medium is the downward energy flux due to an impulsive source at the top of the first layer. A propagation‐invariant form is used to derive several identities for the reflection and transmission matrices. When the top layer is bounded by a free surface, one of the expressions reduces to a formula derived by Kunetz for the one‐dimensional wave equation.
A source radiating upwards and downwards gives a discontinuity in the propagation‐invariant form which is equal to the source energy. A new formula is derived for when the source is located just beneath the top interface of the layers.