A first-order statistical smoothing approximation for the coherent wave field in random porous media
An important dissipation mechanism for waves in randomly inhomogeneous poroelastic media is the effect of wave-induced fluid flow. In the framework of Biot's theory of poroelasticity, this mechanism can be understood as scattering from fast into slow compressional waves. To describe this conver...
| Main Authors: | , |
|---|---|
| Format: | Journal Article |
| Published: |
2005
|
| Online Access: | http://hdl.handle.net/20.500.11937/5805 |