Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
Bulletin of the Seismological Society of America Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Bulletin of the Seismological Society of America; January 1961; v. 51; no. 1; p. 51-59
© 1961 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by DERESIEWICZ, H.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

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.




This article has been cited by other articles:


Home page
 Bulletin of the Seismological Society of AmericaHome page
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]

Home page
 Bulletin of the Seismological Society of AmericaHome page
A. MUKHOPADHYAY
On a moving stress discontinuity in a porous, liquid-saturated solid
Bulletin of the Seismological Society of America, December 1, 1966; 56(6): 1373 - 1385.
[Abstract] [PDF]

Home page
 Bulletin of the Seismological Society of AmericaHome page
H. DERESIEWICZ
The effect of boundaries on wave propagation in a liquid-filled porous solid: IX. Love waves in a porous internal stratum
Bulletin of the Seismological Society of America, October 1, 1965; 55(5): 919 - 923.
[Abstract] [PDF]

Home page
 Bulletin of the Seismological Society of AmericaHome page
H. DERESIEWICZ
The effect of boundaries on wave propagation in a liquid-filled porous solid: VI. Love waves in a double surface layer
Bulletin of the Seismological Society of America, February 1, 1964; 54(1): 417 - 423.
[Abstract] [PDF]

Home page
 Bulletin of the Seismological Society of AmericaHome page
H. DERESIEWICZ and J. T. RICE
The effect of boundaries on wave propagation in a liquid-filled porous solid: III. Reflection of plane waves at a free plane boundary (general case)
Bulletin of the Seismological Society of America, July 1, 1962; 52(3): 595 - 625.
[Abstract] [PDF]


JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Seismological Society of America