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Evaporation – Process , Rate of Evaporation

EVAPORATION

Evaporation is the process in which a liquid changes to the gaseous state at the free surface, below the boiling point through the the transfer of heat energy. Consider a body of water in a pond.

EVAPORATION PROCESS

The molecules of water are in constant motion with a wide range of instantaneous velocities. An addition of heat causes this range and average speed to increase.

When some molecules possess sufficient kinetic energy, they may cross over the water surface. Similarly, the atmosphere in the immediate neighbourhood of the water surface contains water molecules within the water vapour in motion and some of them may penetrate the water surface.

Evaporation




The net escape of water molecules from the liquid state to the gaseous state constitutes evaporation.

Evaporation is a cooling process in that the latent heat of vaporization (at about 585 cal/g of evaporated water) must be provided by the water body.

The rate of evaporation is dependent on  the

(i) vapour pressures at the water surface and air above,

(ii) air and water temperatures,

(iii) wind speed,

(iv) atmospheric pressure,

(v) quality of water and

(vi) size of the water body.

Vapour Pressure:

The  rate  of  evcporation  is  proportional  to  the  difference  between the  saturation vapour pressure at the water temperature, ew  and the actual vapour pressure in the air,ea

Thus

EL = C(ew —ea)

where EL = rate of evaporation (mm I day) and C = a constant; ew and ea are in mm of mercury.

The above equation is known as Dalton’ s law of evaporation after John Dalton (1802) who first recognised this law.

Evaporation continues till ew = ea. If ew > ea    condensation takes place.

Temperature:

Other factors remaining same, the rate of evaporation increases with an increase in the water temperature.

Regarding  air  temperature, although there  is a  general  in crease in the evaporation rate with increasing temperature, a high correlation between evaporation rate and air temperature does not exist.

Thus for the same mean monthly temperature  it  is  possible  to  have  evaporation  to  different  degrees  in  a  lake  in different months.

Wind

Wind aids in removing the evaporated water vapour from the zone of evaporation and consequently creates greater scope for evaporation.

However, if the wind velocity is large enough to remove all the evaporated water vapour, any further increase in wind velocity does not influence the evaporation.

Thus the rate of evaporation increases with the wind speed up to a critical speed beyond which any further increase in the wind speed has no influence on the evaporation rate.

This critical wind-speed value is a  function  of  the  size  of  the  water  surface.  For  large  water  bodies  high-speed turbulent winds are needed to cause maximum rate of evaporation.

Atmospheric Pressure

Other factors remaining same, a decrease in the barometric pressure,  as  in  high altitudes, increases evaporation.

Soluble Salts

When a solute is dissolved in water, the vapour pressure of the solution is less than that of pure water and hence causes reduction in the rate of evaporation.

The percent reduction in evaporation approximately corresponds to the percentage increase in the specific gravity. Thus, for example, under identical conditions evaporation from sea water is about 2-3% less than that from fresh water.

Heat Storage in Water Bodies

Deep water bodies have more heat storage than shallow ones. A deep lake may store radiation energy received in summer and release it in winter causing less evaporation in summer and more evaporation in winter compared to a shallow exposed to  a similar situation.

However, the effect of heat storage is essentially to change the seasonal evaporation rates and the annual evaporation rate is seldom affected.

Other links:

HYDROLOGIC CYCLE
PRECIPITATION
RAIN GAUGE
INFILTRATION
GROUNDWATER
Water Table
AQUIFER PROPERTIES
DARCY’S LAW
FLOOD FREQUENCY STUDIES
RECURRENCE INTERVAL
GUMBEL’S METHOD
FLOOD ROUTING
EVAPORIMETER

 

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