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DEPARTMENT OF MECHANICAL ENGINEERING COLUMBIA UNIVERSITY, NEW YORK, N.Y.
Abstract
The velocity dispersion relation and the expression for the attenuation coefficient are derived appropriate to surface waves in a porous half-space supporting a layer of liquid, generalizing a solution due to Stoneley.
This article has been cited by other articles:
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S. HAJRA and A. MUKHOPADHYAY Reflection and refraction of seismic waves incident obliquely at the boundary of a liquid-saturated porous solid Bulletin of the Seismological Society of America, October 1, 1982; 72(5): 1509 - 1533. [Abstract] [PDF] |
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