Skip Navigation


The Quarterly Journal of Mechanics and Applied Mathematics Advance Access originally published online on October 31, 2008
The Quarterly Journal of Mechanics and Applied Mathematics 2009 62(1):19-30; doi:10.1093/qjmam/hbn022
This Article
Right arrow Full Text (PDF)
Right arrow All Versions of this Article:
62/1/19    most recent
hbn022v1
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
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 Add to My Personal Archive
Right arrow Download to citation manager
Right arrowRequest Permissions
Google Scholar
Right arrow Articles by Parker, D. F.
Right arrow Articles by Kiselev, A. P.
Right arrow Search for Related Content
Social Bookmarking
 Add to CiteULike   Add to Connotea   Add to Del.icio.us  
What's this?

© The author 2008. Published by Oxford University Press; all rights reserved. For Permissions, please email: journals.permissions@oxfordjournals.org

Rayleigh waves having generalised lateral dependence

D. F. Parker{dagger}

( School of Mathematics, University of Edinburgh, Edinburgh EH9 3JZ )

A. P. Kiselev

( St. Petersburg Branch, Steklov Institute of Mathematics, St. Petersburg, 191023 Russia )

{dagger} <d.f.parker{at}ed.ac.uk>

Received 22 April 2008. Revise 30 September 2008.
   Abstract

It is shown that the surface-guided elastic waves found by Kiselev for isotropic materials and having displacements depending linearly upon the Cartesian coordinate orthogonal to the sagittal plane may be generalised in many ways. For surface waves on any anisotropic half-space, a simple procedure applied to the displacements within the standard surface wave having dependence ei{theta}, where {theta} {equiv} k · x{omega}t and k is the (surface) wave vector, yields displacements depending linearly upon the surface cartesian coordinate orthogonal to the group velocity vector. Moreover, repeated application of this (differentiation) procedure yields a hierarchy of waves having algebraic dependence of successively increasing degree. For isotropic materials, substantial simplification and generalization are possible. Solutions of all algebraic degrees have identical depth dependence. This allows the solutions to be constructed iteratively and motivates a search for general solutions having depth dependence of the normal displacement the same as in the standard surface wave. The procedure gives a new derivation of the solutions found by Achenbach having amplitude of the normal displacement of the surface given by any solution to the two-dimensional Helmholtz equation. Furthermore, exploiting the scale invariance (a property of surface waves on any homogeneous half-space) shows that in every surface-guided disturbance of an elastic half-space, the elevation of the free surface is a solution of the wave equation in two dimensions (the membrane equation). Using the paraxial approximation to the membrane equation, high-frequency Rayleigh waves propagating as narrow beams are described in terms of a scalar Gaussian beam.


Add to CiteULike CiteULike   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us    What's this?




Disclaimer: Please note that abstracts for content published before 1996 were created through digital scanning and may therefore not exactly replicate the text of the original print issues. All efforts have been made to ensure accuracy, but the Publisher will not be held responsible for any remaining inaccuracies. If you require any further clarification, please contact our Customer Services Department.