During the winter (rabi) season in central India, dryland crops rely on stored soil water and limited precipitation. Crop evaporation rates were calculated from changes in soil moisture content under wheat, dhal, lentil, linseed and mixed crops during periods of little or no rainfall. Seasonal varia
The evaporation of moisture from wet surfaces
β Scribed by J.C. Ashworth; R.B. Keey
- Publisher
- Elsevier Science
- Year
- 1972
- Tongue
- English
- Weight
- 773 KB
- Volume
- 27
- Category
- Article
- ISSN
- 0009-2509
No coin nor oath required. For personal study only.
β¦ Synopsis
The authors investigate "exact" relationships for the flux of vapour leaving a wet surface in terms of the humidity potential and wet-bulb depression. As the wet-bulb temperature rises the departure from a linear relationship becomes more marked, but the flux is still directly proportional to the humidity potential for processes at a constant wet-bulb temperature. The difference between the wet-bulb and adiabatic-saturation temperatures is shown to decrease with increasing wet-bulb temperature and vanish altogether at the boiling point. A new humidity chart, based on the "exact" relationships developed, is presented which yields a greater reading accuracy than charts of similar size hitherto produced.
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