Difference between revisions of "Condensation" - New World Encyclopedia
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[[Image:watervapor_cup.jpg|right|thumb|Water condenses into visible droplets after evaporating from a cup of hot tea.]] | [[Image:watervapor_cup.jpg|right|thumb|Water condenses into visible droplets after evaporating from a cup of hot tea.]] | ||
| − | '''Condensation''' is the change in | + | '''Condensation''' is the change in phase of a substance from a [[gas]] (or vapor) to a [[liquid]].<ref>{{GoldBookRef|title=condensation ''in atmospheric chemistry''|file=C01235}}</ref> It occurs when a vapor is cooled or compressed or subjected to both cooling and compression.<ref>Compression of a vapor means that the [[pressure]] on it is increased.</ref> For example, the water seen on the outside of a cold glass on a hot day is condensation. |
| − | + | Liquid that is formed by condensation of a vapor is called the '''condensate''', and a device or unit used to condense vapors is called a '''[[condenser]]'''. Condensers are used in [[heat exchanger]]s of various designs and come in many sizes, ranging from small (hand-held) devices to very large. | |
==Condensation of water in nature== | ==Condensation of water in nature== | ||
| − | [[Image:Water drops on spider web.jpg|left|thumb|[[Dew]] on a spider web]] | + | [[Image:Water drops on spider web.jpg|left|thumb|[[Dew]] on a spider web.]] |
| − | + | When water vapor from the air naturally condenses on cold surfaces into liquid water, it is called '''[[dew]]'''. Condensation of water vapor within the [[Earth's atmosphere|atmosphere]] produces [[cloud]]s. | |
| − | + | Water vapor will only condense onto another surface when that surface is cooler than the [[temperature]] of the water vapor, or when the saturation [[humidity]] of the vapor in the air has been exceeded. When water vapor condenses onto a surface, the water releases some heat onto the surface, which becomes slightly warmer. At the same time, the temperature of the [[atmosphere]] drops very slightly. | |
| − | Also, a net condensation of water vapor occurs on surfaces when the temperature of the surface is at or below the dew point temperature of the atmosphere | + | [[Image:Condensation_on_water_bottle.jpg|200px|thumb|Condensation on a cold [[Bottled Water|bottle of water]].]] |
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| + | The "[[dew point]]" of an air parcel is the temperature to which it must cool before condensation in the air begins to form. Also, a net condensation of water vapor occurs on surfaces when the temperature of the surface is at or below the dew point temperature of the atmosphere. [[Deposition (physics)|Deposition]], the direct formation of ice from water vapor, is a type of condensation. Frost and [[snow]] are examples of deposition. | ||
=== Condensation in buildings === | === Condensation in buildings === | ||
| − | Condensation is the most common form of dampness encountered in buildings. In buildings the internal air can have a high level of relative humidity due to | + | Condensation is the most common form of dampness encountered in buildings. In buildings, the internal air can have a high level of relative humidity due to the occupants' activities such as cooking, drying clothes, and even breathing. When this air comes into contact with cold surfaces such as windows and cold walls it can condense, causing dampness.<ref>http://www.buildingpreservation.com/Condensation.htm Building Preservation (Condensation - the basics)</ref> |
== Applications of condensation == | == Applications of condensation == | ||
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Condensation is a crucial component of [[distillation]], an important application in laboratory and industrial chemistry application. | Condensation is a crucial component of [[distillation]], an important application in laboratory and industrial chemistry application. | ||
| − | Because condensation is a naturally occurring phenomenon, it can often be used to generate | + | Because condensation is a naturally occurring phenomenon, it can often be used to generate large quantities of water for human use. Many structures—such as [[fog fence]]s, [[air well]]s, and [[dew pond]]s—are made solely for the purpose of collecting water from condensation. Such systems can be used to retain soil moisture in areas where active [[desertification]] is occurring. Some organizations provide education programs about water condensers in efforts to effectively aid such areas.<ref>http://www.fogquest.org/</ref> |
==See also== | ==See also== | ||
Revision as of 21:53, 23 September 2007
- For other uses, see Condensation (disambiguation).
Condensation is the change in phase of a substance from a gas (or vapor) to a liquid.[1] It occurs when a vapor is cooled or compressed or subjected to both cooling and compression.[2] For example, the water seen on the outside of a cold glass on a hot day is condensation.
Liquid that is formed by condensation of a vapor is called the condensate, and a device or unit used to condense vapors is called a condenser. Condensers are used in heat exchangers of various designs and come in many sizes, ranging from small (hand-held) devices to very large.
Condensation of water in nature
When water vapor from the air naturally condenses on cold surfaces into liquid water, it is called dew. Condensation of water vapor within the atmosphere produces clouds.
Water vapor will only condense onto another surface when that surface is cooler than the temperature of the water vapor, or when the saturation humidity of the vapor in the air has been exceeded. When water vapor condenses onto a surface, the water releases some heat onto the surface, which becomes slightly warmer. At the same time, the temperature of the atmosphere drops very slightly.
The "dew point" of an air parcel is the temperature to which it must cool before condensation in the air begins to form. Also, a net condensation of water vapor occurs on surfaces when the temperature of the surface is at or below the dew point temperature of the atmosphere. Deposition, the direct formation of ice from water vapor, is a type of condensation. Frost and snow are examples of deposition.
Condensation in buildings
Condensation is the most common form of dampness encountered in buildings. In buildings, the internal air can have a high level of relative humidity due to the occupants' activities such as cooking, drying clothes, and even breathing. When this air comes into contact with cold surfaces such as windows and cold walls it can condense, causing dampness.[3]
Applications of condensation
Condensation is a crucial component of distillation, an important application in laboratory and industrial chemistry application.
Because condensation is a naturally occurring phenomenon, it can often be used to generate large quantities of water for human use. Many structures—such as fog fences, air wells, and dew ponds—are made solely for the purpose of collecting water from condensation. Such systems can be used to retain soil moisture in areas where active desertification is occurring. Some organizations provide education programs about water condensers in efforts to effectively aid such areas.[4]
See also
Notes
- ↑ International Union of Pure and Applied Chemistry. "condensation in atmospheric chemistry". Compendium of Chemical Terminology Internet edition.
- ↑ Compression of a vapor means that the pressure on it is increased.
- ↑ http://www.buildingpreservation.com/Condensation.htm Building Preservation (Condensation - the basics)
- ↑ http://www.fogquest.org/
ReferencesISBN links support NWE through referral fees
External links
From To Solid Liquid Gas Plasma Solid Solid-Solid Transformation Melting Sublimation - Liquid Freezing N/A Boiling/Evaporation - Gas Deposition Condensation N/A Ionization Plasma - - Recombination/Deionization N/A
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