EVAPORATION

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evaporation

Evaporation is nothing but a thermal separation process. Theoretically, evaporation means simply vaporization from the surface of a liquid. Vaporization of a liquid below its boiling point is called evaporation. Thus, no boiling occurs and the rate of vaporization depends on the diffusion of vapour through the boundary layers above the liquid.:

Evaporation is nothing but a thermal separation process. Theoretically, evaporation means simply vaporization from the surface of a liquid. Vaporization of a liquid below its boiling point is called evaporation. Thus, no boiling occurs and the rate of vaporization depends on the diffusion of vapour through the boundary layers above the liquid . DEFINiTION AND PRINCIPLE OF EVAPORATION

There are 4 factors to affect evaporation. 1) Temperature 2) Surface area 3) HUMIDITY 4)WIND SPEED :

There are 4 factors to affect evaporation. 1) Temperature 2) Surface area 3) HUMIDITY 4)WIND SPEED Factors Affecting Evaporation

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Temperature It is also affected by temperature. As the temperature of air is increased, its capacity to hold moisture also increases. Any increase in air temperature raises the temperature of water at the evaporation source which means that more energy is available to the water molecules for escaping from liquid to a gaseous state. Hence evaporation is directly proportional to the temperature of evaporating surface. Warmer the evaporating surface, higher the rate of evaporation

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The rate of evaporation is closely related with the relative humidity of air. Since the moisture holding capacity of air at a given temperature is limited, drier air evaporates more water than moist air . In other words, higher the vapour pressure, lower the rate of evaporation. It is a common experience that evaporation is greater in summer and at mid-day than in winter and at night. Humidity

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Wind Speed Evaporation depends on the wind speed as well. When the winds are light, a thin layer of air just above the surface gets nearly saturated; under the circumstances the difference between the vapour pressure between ground and air is very small . This results in very low evaporation. On the other hand, when the wind velocity is high, turbulence is set up in the air. Moisture evaporated from the ground is mixed upward and the vapour -pressure difference between the atmosphere and the surface remains large. Thus, the rate of evaporation is accelerated. Wherever there is a combination of high temperature, very low relative humidity and strong wind, the rate of evaporation is exceptionally high.

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Surface Area The rate of evaporation is determined by the area of the exposed surface of water. Larger areas of evaporating surface increase the rate of evaporation.

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