The Motion of the Surface of a Uniform Elastic Half‐Space Produced by a Buried Torque‐Pulse

12Citations
Citations of this article
6Readers
Mendeley users who have this article in their library.
Get full text

Abstract

In this investigation we determine the motion of the surface of a uniform elastic half‐space produced by the application of a torque‐pulse at a point below the surface. The axis of the torque is taken to be parallel to the surface and its time variation is assumed to be represented by the Heaviside unit function H(t). Our results are compared with those of Pinney (1954), who treated the same problem by a different method. The principal feature of physical interest which we found is that, for ranges where the direct S wave is preceded by a diffracted SP wave, the displacement at the surface starts with an infinite amplitude at the time of arrival of the SP wave, and that this is followed by an even stronger infinity at the time of arrival of the S wave. Also, for small ranges, for which there is no SP wave, the displacement starts with a sharp pulse in the form of a Dirac delta function. None of these features was brought out by Pinney's curves. The results are shown in Figures 2, 3 and 4. Copyright © 1958, Wiley Blackwell. All rights reserved

Cite

CITATION STYLE

APA

Pekeris, C. L., & Longman, I. M. (1958). The Motion of the Surface of a Uniform Elastic Half‐Space Produced by a Buried Torque‐Pulse. Geophysical Journal of the Royal Astronomical Society, 1(2), 146–153. https://doi.org/10.1111/j.1365-246X.1958.tb00045.x

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free