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Bulletin of the Seismological Society of America; January 1961; v. 51; no. 1; p. 51-59
© 1961 Seismological Society of America
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The effect of boundaries on wave propagation in a liquid-filled porous solid: II. Love waves in a porous layer

H. DERESIEWICZ

DEPARTMENT OF MECHANICAL ENGINEERING, COLUMBIA UNIVERSITY,, NEW YORK, N. Y.

Abstract

The transcendental equation is derived relating frequency and phase velocity of propagation of Love waves in a porous layer containing a viscous liquid. This equation, being complex, can be satisfied only if the wave number of the motion is complex, indicating that the disturbance is dissipative.

The general expression being intractable analytically, an approximate scheme is employed to determine the phase velocity and measure of dissipation valid for porous materials in which the mass (per unit volume of aggregate) of the interstitial liquid is smaller than that of the solid.

Footnotes

This investigation was supported by National Science Foundation Grant NSF-G10242.




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