Diffusion advection is an effect in diffusive multicomponent mass transfer that occurs when the flux vectors of the individual components do not add up to zero. This can be a significant effect for the mass transfer of water vapor from subsurface ice or liquid reservoirs through porous regolith at m
The analysis of water in the Martian regolith
β Scribed by D. M. Anderson; A. R. Tice
- Publisher
- Springer
- Year
- 1979
- Tongue
- English
- Weight
- 357 KB
- Volume
- 14
- Category
- Article
- ISSN
- 0022-2844
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