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Purpose:In this experiment, we will use the Humidity/Temp/Dew Point Sensor to measure air temperature, dew point and relative humidity in a plant terrarium. Well then hypothesize reasons for any changes.Background Information:The amount of water vapor in the air is called humidity. As water molecules evaporate, the humidity of the air increases. Certain climate regions on earth (such as deserts, Arctic and Antarctic regions) have very low humidity, while other climate regions (such as tropical rain forests) have moderate to high humidity. In general, the amount of water vapor that a given volume of air can hold increases as the temperature increases. A higher temperature allows more water to evaporate into water vapor. As the temperature goes down, the amount of water vapor in the air goes down because the water vapor molecules can condense into liquid form again. Therefore, the humidity drops. When the air holds all the water vapor it can at a given temperature, the air is saturated. The point at which saturation occurs is called the dew point. Relative humidity is a common way to describe the amount of water vapor in the air. Relative humidity is a ratio that compares the mass of water vapor in the air to the mass of water vapor that the air can hold at its saturation point. Relative humidity is always written as a percentage. For example, the average relative humidity in the
rainforest is high, typically ranging from 75% to 95%. Equipment:For each lab group:
Software Setup:
Experimental Procedure:Data Recording:
Data Analysis:
Conclusions and Extensions:
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