Condensation

Source: Wikipedia, the free encyclopedia.
For other uses, see Condensation (disambiguation).
Condensation forming in the low pressure zone above the wing of an aircraft due to adiabatic expansion

Condensation is the change of the

atmosphere. When the transition happens from the gaseous phase into the solid phase directly, the change is called deposition
.

Initiation

Condensation is initiated by the formation of

clouds, this can be catalyzed by water-nucleating proteins
, produced by atmospheric microbes, which are capable of binding gaseous or liquid water molecules. [2]

Reversibility scenarios

A few distinct reversibility scenarios emerge here with respect to the nature of the surface.

  • absorption into the surface of a liquid (either of the same substance or one of its solvents)—is reversible as evaporation.[1]
  • adsorption (as dew droplets) onto solid surface at pressures and temperatures higher than the species' triple point—also reversible as evaporation.
  • adsorption onto solid surface (as supplemental layers of solid) at pressures and temperatures lower than the species'
    sublimation
    .

Most common scenarios

Condensation commonly occurs when a vapor is cooled and/or compressed to its saturation limit when the molecular density in the gas phase reaches its maximal threshold. Vapor cooling and compressing equipment that collects condensed liquids is called a "condenser".

Condensation on the outside of a window, due to it being in front of the sea which regularly produces moist sea spray.

Measurement

Psychrometry
measures the rates of condensation through evaporation into the air moisture at various atmospheric pressures and temperatures. Water is the product of its vapor condensation—condensation is the process of such phase conversion.

Applications of condensation

contrails

Condensation is a crucial component of distillation, an important laboratory and industrial chemistry application.

Because condensation is a naturally occurring phenomenon, it can often be used to generate water in large quantities for human use. Many structures are made solely for the purpose of collecting water from condensation, such as

fog fences. Such systems can often be used to retain soil moisture in areas where active desertification is occurring—so much so that some organizations educate people living in affected areas about water condensers to help them deal effectively with the situation.[3]

It is also a crucial process in forming particle tracks in a cloud chamber. In this case, ions produced by an incident particle act as nucleation centers for the condensation of the vapor producing the visible "cloud" trails.

Commercial applications of condensation, by consumers as well as industry, include power generation, water desalination,[4] thermal management,[5] refrigeration,[6] and air conditioning.[7]

Biological adaptation

Numerous living beings use water made accessible by condensation. A few examples of these are the Australian thorny devil, the darkling beetles of the Namibian coast, and the coast redwoods of the West Coast of the United States.

Condensation in building construction

Condensation on a window during a rain shower.

Condensation in building construction is an unwanted phenomenon as it may cause dampness, mold health issues, wood rot, corrosion, weakening of mortar and masonry walls, and energy penalties due to increased heat transfer. To alleviate these issues, the indoor air humidity needs to be lowered, or air ventilation in the building needs to be improved. This can be done in a number of ways, for example opening windows, turning on extractor fans, using dehumidifiers, drying clothes outside and covering pots and pans whilst cooking. Air conditioning or ventilation systems can be installed that help remove moisture from the air, and move air throughout a building.[8] The amount of water vapor that can be stored in the air can be increased simply by increasing the temperature.[8] However, this can be a double edged sword as most condensation in the home occurs when warm, moisture heavy air comes into contact with a cool surface. As the air is cooled, it can no longer hold as much water vapor. This leads to deposition of water on the cool surface. This is very apparent when central heating is used in combination with single glazed windows in winter.

Interstructure condensation may be caused by thermal bridges, insufficient or lacking insulation, damp proofing or insulated glazing.[9]

Table

Phase transitions of matter (
)
To
From
 Solid Liquid Gas Plasma
Solid
Melting Sublimation
Liquid Freezing
Vaporization
Gas Deposition Condensation
Ionization
Plasma Recombination

See also

References

  1. ^
    doi:10.1351/goldbook.C01235
  2. ^ Schieormeier, Quirin (2008-02-28). "'Rain-making' bacteria found around the world". Nature. Retrieved 2018-06-21.
  3. ^ FogQuest - Fog Collection / Water Harvesting Projects - Welcome Archived 2009-02-23 at the Wayback Machine
  4. doi:10.3390/e17117530
    .
  5. ^ White, F.M. ‘Heat and Mass Transfer’ © 1988 Addison-Wesley Publishing Co. pp. 602–604
  6. ^ Q&A: Microchannel air-cooled condenser; Heatcraft Worldwide Refrigeration; April 2011; "Archived copy" (PDF). Archived (PDF) from the original on 2012-04-17. Retrieved 2013-02-20.{{cite web}}: CS1 maint: archived copy as title (link)
  7. S2CID 97855214. Archived
    (PDF) from the original on 2019-09-23.
  8. ^ a b "Condensation". Property Hive. Archived from the original on 2013-12-13.
  9. ^ "Condensation around the house - what causes condensation". diydata.com. Archived from the original on 2008-01-13.
Sources
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