Condensation occurs when the molecules of a gas cool. The molecules lose energy and slow down as they lose heat. They approach other gas molecules and combine to form a liquid.
On the other hand, the process of a liquid becoming a gas is called vapourization.
Some examples of condensation reactions are listed below:
- When water droplets in clouds combine, they become heavy enough to form raindrops that fall from the sky.
- Fog shows up when water vapor, or water in its gaseous form, condenses.
- Dew is the moisture that forms as a result of condensation.
Table of Contents
Condensation Definition
Condensation is the transition of matter from the gas to the liquid phase.
Condensation takes place. When gas molecules transfer their energy to something cooler, they slow down, and their attractions cause them to bond, resulting in the formation of a liquid.
Making water vapor colder accelerates condensation.
The rate of condensation increases as the concentration of water vapor in the air increases.
Role of Condensation in Water Cycle
Condensation is necessary for the water cycle because it causes clouds to form. These clouds may produce precipitation within the water cycle, which is the primary route for water to return to the Earth’s surface. Condensation’s inverse is evaporation.
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