## Abstract The linear and non‐linear stability of a horizontal layer of a binary fluid mixture in a porous medium heated and salted from below is studied, in the Oberbeck–Boussinesq–Darcy scheme, through the Lyapunov direct method. This is an interesting geophysical case because the salt gradient
Non-linear diffusion in a finite mass medium
✍ Scribed by P. Rosenau; S. Kamin
- Publisher
- John Wiley and Sons
- Year
- 1982
- Tongue
- English
- Weight
- 461 KB
- Volume
- 35
- Category
- Article
- ISSN
- 0010-3640
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