Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Bulletin of the Seismological Society of America; October 1979; v. 69; no. 5; p. 1409-1423
© 1979 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
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 CHEN, T. C.
Right arrow Articles by ALSOP, L. E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Reflection and transmission of obliquely incident Rayleigh waves at a vertical discontinuity between two welded quarter-spaces

THOMAS C. CHEN and LEONARD E. ALSOP

LAMONT-DOHERTY GEOLOGICAL OBSERVATORY AND DEPARTMENT OF GEOLOGICAL SCIENCES COLUMBIA UNIVERSITY, PALISADES, NY 10964
IBM THOMAS J. WATSON RESEARCH CENTER, YORKTOWN HEIGHTS, NEW YORK 10598

Abstract

We use an approximate method to study the reflection and transmission of obliquely incident Rayleigh waves on a vertical boundary between two welded quarter-spaces. For two media with a phase velocity ratio of 1.16 our calculation shows that the transmitted energy follows a reciprocity relation and decreases from near 100 per cent at normal incidence to 50 per cent at about 40°. The reflected energy is less than 1 per cent for angles of reflection less than 40°. When the Rayleigh wave impinges upon the less rigid medium, the reflected energy decreases as the angle of incidence increases; whereas for incidence at the more rigid medium, the reflected energy decreases at first, and then it increases as the angle of incidence increases. Since boundary conditions on the free surface are not taken into account by our method, diffraction effects are ignored. The effect of neglecting the free surface requirement is difficult to quantify, but we believe that it is small since the calcualted and experimental results agree well at normal incidence.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
J. T. BULLITT and M. N. TOKSOZ
Three-dimensional ultrasonic modeling of Rayleigh wave propagation
Bulletin of the Seismological Society of America, August 1, 1985; 75(4): 1087 - 1104.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
J. W. SCHLUE
Seismic surface wave propagation in three-dimensional finite-element structures
Bulletin of the Seismological Society of America, August 1, 1981; 71(4): 1003 - 1010.
[Abstract] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1979 by the Seismological Society of America.