Evaporation from bare soil proceeds in three stages as the soil surface dries. The formation of a dry surface layer (DSL), where water moves only in the vapour phase, is the most remarkable and symbolic feature of the last stage, and the following phenomena, observed recently, seem to be closely rel
โฆ LIBER โฆ
Effect of sand shape on evaporation from soil surface
โ Scribed by N. D. Misopolinos; J. M. Kalovoulos
- Publisher
- Springer
- Year
- 1984
- Tongue
- English
- Weight
- 153 KB
- Volume
- 80
- Category
- Article
- ISSN
- 0032-079X
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## Abstract The understanding of soil water repellency in its complexity requires knowledge of the mechanisms leading to changes in surface characteristics. Wetting kinetics may serve as means to investigate the origin of soil water repellency, but have been scarcely investigated yet. We observe th