SH-wave propagation in a viscoelastic sandy layer lying over an anisotropic half space is investigated. Imperfect interface is considered. The problem consists of determining displacement field and then obtaining frequency equation for SH-wave in closed form by adopting variable separation method. Effects of parameters like imperfection, sandiness, dissipation factor on phase velocity is examined by analyzing dispersion equation graphically. MATLAB software has been used to plot the graphs. The present study may find useful applications in earthquake engineering, geophysics and civil engineering.
| Published in | Abstract Book of the National Conference on Advances in Basic Science & Technology |
| Page(s) | 99-99 |
| Creative Commons |
This is an Open Access abstract, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited. |
| Copyright |
Copyright © The Author(s), 2025. Published by Science Publishing Group |
Anisotropic, Dissipation Factor, Imperfect, Sandiness, SH-wave, Viscoelastic Sandy
Information
Share This Abstract
Twitter
Linked In
Facebook