Condensation: Difference between revisions
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== Condensation == | |||
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File:Cloud_over_A340_wing.JPG|Cloud over A340 wing | |||
File:Condensation_on_outside_of_windows.png|Condensation on outside of windows | |||
File:Effect_similar_to_contrails_created_in_a_cloud_chambers.jpg|Effect similar to contrails created in a cloud chamber | |||
File:Window_in_Ireland.jpg|Condensation | |||
</gallery> | |||
Latest revision as of 04:57, 18 February 2025
Condensation is a physical process in which a gas or vapor changes its state to a liquid. This process is crucial in various fields such as meteorology, chemistry, and physics.
Overview[edit]
Condensation occurs when the molecules of a gas cool down and lose kinetic energy. As a result, the molecules slow down and come closer together, forming a liquid. This process is the opposite of evaporation, where a liquid turns into a gas.
Process[edit]
The process of condensation involves the cooling of a gas until it reaches its dew point, or the temperature at which the gas becomes saturated and condenses into a liquid. This can occur naturally, such as when water vapor in the air condenses to form dew or fog, or it can be induced artificially in industrial processes.
Applications[edit]
Condensation has numerous applications in various fields. In meteorology, it is responsible for the formation of clouds and precipitation. In chemistry, it is used in condensation reactions, where two molecules combine to form a larger molecule, often producing a small molecule such as water as a byproduct. In physics, it is studied in the field of thermodynamics.
See also[edit]
References[edit]
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