Attenuation and dispersion of elastic waves in porous rocks : mechanisms and models /
Wave propagation in all fluid and solid matter is always accompanied by attenuation and dispersion in a broad range of frequencies and scales from free oscillations of the entire Earth to ultrasound in small rock samples. Attenuation is the exponential decay of wave amplitude with propagation distan...
| Main Authors: | , |
|---|---|
| Format: | Book |
| Language: | English |
| Published: |
Houston :
Society of Explorations Geophysicists,
[2022].
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| Series: | Geophysical references ;
no. 26. |
| Subjects: |
Table of Contents:
- About the authors
- Preface
- Basic notation
- Viscoelasticity and wave propagation
- The Biot theory of dynamic poroelasticity
- Mesoscopic-flow relaxation
- Patchy saturation
- Pressure relaxation between pores and fractures
- Pore-scale (squirt) flow relaxation
- Rocks with solid and viscoelastic pore fill
- Rigorous bounds for dispersion and attenuation
- Appendix A: Effective properties of inhomogeneous media
- Appendix B: Laboratory methods for measurements of attenuation and dispersion.