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
The equations of motion in porous media
β Scribed by S. Whitaker
- Publisher
- Elsevier Science
- Year
- 1966
- Tongue
- English
- Weight
- 752 KB
- Volume
- 21
- Category
- Article
- ISSN
- 0009-2509
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β¦ Synopsis
Ah&act-The continuity equation and the equations of motion are developed for flow in anisotropic porous media, and the conditions under which Darcy's law holds are clearly established.
π SIMILAR VOLUMES
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