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: | Muller, T., Caspari, E., Qi, Q., Rubino, J., Velis, D., Lopes, S., Lebedev, Maxim, Gurevich, Boris |
|---|---|
| Format: | Book Chapter |
| Published: |
Elsevier Inc.
2015
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| Online Access: | http://hdl.handle.net/20.500.11937/24902 |
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