| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 10736131 | Wave Motion | 2005 | 17 Pages |
Abstract
One important result of this work is that the introduction of the two parameters p and pâ² corrects the Johnson-Allard model by increasing attenuation with no change in dispersion. This phenomenon is much more significant for resistive porous materials.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Z.E.A. Fellah, C. Depollier, M. Fellah, W. Lauriks, J.-Y. Chapelon,