Propagation of acoustic waves in unsaturated porous media
โ Scribed by A. M. Maksimov
- Book ID
- 110623456
- Publisher
- Springer US
- Year
- 1998
- Tongue
- English
- Weight
- 503 KB
- Volume
- 71
- Category
- Article
- ISSN
- 1573-871X
No coin nor oath required. For personal study only.
๐ SIMILAR VOLUMES
The equations of soil freezing are established where the soil is partially water-saturated, i.e., when it contains air. We choose a macroscopic viewpoint, using leveled parameters (averages on a "small" volume surrounding the considered point). We assume that water can exist at a temperature below 0
Some ocean sediments may be modeled as poro-elastic media with relatively high slow-wave speeds and relatively low shear-wave speeds [NJ? Chotiros, "Biot model of sound propagation in water-saturated sand", J. Acoust. Sot. Amer 97, 199-214 (1995)]. This singular limit may be handled efficiently by a