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; June 1969; v. 59; no. 3; p. 1349-1364
© 1969 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
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by MCIVOR, I. K.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Two-dimensional scattering of a plane compressional wave by surface imperfections

IVOR K. MCIVOR

GEOPHYSICS LABORATORY WILLOW RUN LABORATORIES INSTITUTE OF SCIENCE AND TECHNOLOGY UNIVERSITY OF MICHIGAN, ANN ARBOR

Abstract

A perturbation method for treating the scattering of plane waves by small surface imperfections on an elastic half space is presented. The solution to the first order approximation is given as convolution integrals of the surface imperfection with kernel functions defined by Fourier inversion integrals. The evaluation of these integrals is discussed and their asymptotic representations determined. The far field scattered displacements are explicitly obtained for arbitrary imperfections. The scattered field consists of a Rayleigh surface wave and four body phases which at the free surface travel with the speed of dilational or distortional waves. Numerical examples are given. In particular the error in the apparent angle of emergence due to the scattered waves is obtained. The body phases exhibit the familiar 3/2 geometric attenuation, but still may make a significant contribution at moderately long distances. A strong dependence of the magnitude of the error on the angle of incidence is demonstrated.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
R. H. Clouser and C. A. Langston
Modeling P-Rg conversions from isolated topographic features near the NORESS array
Bulletin of the Seismological Society of America, June 1, 1995; 85(3): 859 - 873.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
F. J. SANCHEZ-SESMA, M. A. BRAVO, and I. HERRERA
Surface motion of topographical irregularities for incident P, SV, and Rayleigh waves
Bulletin of the Seismological Society of America, February 1, 1985; 75(1): 263 - 269.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
F. J. SANCHEZ-SESMA
Diffraction of elastic waves by three-dimensional surface irregularities
Bulletin of the Seismological Society of America, December 1, 1983; 73(6A): 1621 - 1636.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
M. BOUCHON
Effect of topography on surface motion
Bulletin of the Seismological Society of America, April 1, 1973; 63(2): 615 - 632.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
D. M. BOORE
A note on the effect of simple topography on seismic SH waves
Bulletin of the Seismological Society of America, February 1, 1972; 62(1): 275 - 284.
[Abstract] [PDF]




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