Condensation
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 | edit source]
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 | edit source]
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 | edit source]
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 | edit source]
References[edit | edit source]
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Contributors: Prab R. Tumpati, MD