Physics – Geophysics
Scientific paper
2007-11-28
Proceedings of the Royal Society of London A463 (2007) 495-502
Physics
Geophysics
8 pages
Scientific paper
10.1098/rspa.2006.1774
Efforts at modelling the propagation of seismic waves in half-spaces with continuously varying properties have been mostly focused on shear-horizontal waves. Here a sagittaly polarized (Rayleigh type) wave travels along a symmetry axis (and is attenuated along another) of an orthotropic material with stiffnesses and mass density varying in the same exponential manner with depth. Contrary to what could be expected at first sight, the analysis is very similar to that of the homogeneous half-space, with the main and capital difference that the Rayleigh wave is now dispersive. The results are illustrated numerically for (i) an orthotropic half-space typical of horizontally layered and vertically fractured shales and (ii) for an isotropic half-space made of silica. In both examples, the wave travels at a slower speed and penetrates deeper than in the homogeneous case; in the second example, the inhomogeneity can force the wave amplitude to oscillate as well as decay with depth, in marked contrast with the homogeneous isotropic general case.
No associations
LandOfFree
Seismic Rayleigh waves on an exponentially graded, orthotropic half-space does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Seismic Rayleigh waves on an exponentially graded, orthotropic half-space, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Seismic Rayleigh waves on an exponentially graded, orthotropic half-space will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-45171