Acoustics of Partially Saturated Rocks: Theory and Experiments
The presence of fluids in the pore space of rocks causes wave attenuation and dispersion by the mechanism broadly known as wave-induced fluid flow (WIFF). WIFF occurs as a seismic wave that creates pressure gradients within the fluid phase, and the resulting oscillatory movement of the fluid relativ...
| Main Authors: | , , , , , , , |
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| Format: | Book Chapter |
| Published: |
Elsevier Inc.
2015
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| Online Access: | http://hdl.handle.net/20.500.11937/24902 |