Activity Based Science Learning >Measure dew point in your room


Objective: To measure dew point.
Equipment:
Two steel glasses preferably new ones with shining surfaces, Cold water in a separate bottle, laboratory thermometer measuring up to 500C.
Introduction:
Air in our surrounding contains water vapour. In general the amount of vapour in a given volume of air is less than that required to saturate it. That is why wet cloths dry, water kept in a shallow plate evaporates and so on. The amount of vapour needed to saturate the air depends on temperature. At higher temperature, larger amount of vapour in needed to saturate the air than that needed at lower temperature. If the temperature of the air in your room is decreased sufficiently, the existing amount of vapour will become sufficient to saturate it. If the air is further cooled the existing amount of vapour will become more than that needed to saturate the air and then some vapour will condense to liquid water. This is what happens during the winter nights in open fields. The water that appears on grass or other objects is called Dew. The temperature at which the existing vapour in air will saturate it is called the “Dew point”. Evidently, the dew point will vary with place and time. During rainy season there is lot of vapour in air and the due point will be high. During dry seasons the dew point will be low as there will be only small amount of vapour present in air.
The amount of vapour present in air is often represented by the pressure exterted by the vapour molecules. This is known as  vapour pressure. If the air is saturated with the vapour the vapour pressure is called saturation vapour pressure. The saturation vapour pressure at different temperatures have been measured carefully and tables are available to give these data. If you know the dew point, you can immediately calculate the relative humidity by the relation

Relative humidity = (saturation vapour pressure at dew point)/( saturation vapour pressure at the existing air temperature).
Procedure:
Put two steel glasses side by side. Keep cold water, taken from a refrigerator or water cooler in a bottle or a jug. It should be cold enough so that you can see large water drops on the outer surface of the bottle. Fill one of the steel gasses with  normal tap water up to say one-fourth of its height. Put the thermometer in the water. Ask some one to keep looking at the outer surfaces of the two glasses.
Pour a small amount of cold water in the water, stir with the thermometer  and ask the person looking at the glasses if she/he can see a difference in the shining of the two glasses. If not pour some more cold water and repeat the observation. When the difference in shining is observed read the thermometer. This is the dew point.
Steel is a good conductor of heat and the thickness of the wall is also quite small. So the temperature of the outer surface of the glass, up to the height of the water, quickly becomes the same as that of the water inside. The air in contact with this part of the steel surface also cools down and attains this temperature. When the temperature falls to the dew point and goes slightly below it, vapour in this part of the air starts condensing and small droplets collect on the glass surface. By comparing the two glasses kept side by side, you can easily make out when this condensation has just started. So the dew point can be easily obtained.
Using the saturation vapour pressure table, find the relative humidity.
Discussion:
The dew point can be measured very accurately using this procedure. If your thermometer reads up to half a degree and you do the experiment carefully, you can get the dew point within the accuracy of half degree. Make sure that your initial water in cold enough. The test is that water drops are very clearly seen on the outer surface of the vessel containing the cold water. You can first do a rough experiment to get an estimate of the dew point and then do a fine experiment by varyuing the mixture temperature in that vicinity to get more accurate value.
Instrument cost and availability:
Laboratory thermometer available in any scientific store.



 


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