Advertisement

Advertisement

adiabatic

[ ad-ee-uh-bat-ik, ey-dahy-uh- ]

adjective

  1. occurring without gain or loss of heat ( diabatic ):

    an adiabatic process.



adiabatic

/ ˌeɪ-; ˌædɪəˈbætɪk /

adjective

  1. (of a thermodynamic process) taking place without loss or gain of heat
“Collins English Dictionary — Complete & Unabridged” 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012


noun

  1. a curve or surface on a graph representing the changes in two or more characteristics (such as pressure and volume) of a system undergoing an adiabatic process
“Collins English Dictionary — Complete & Unabridged” 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

adiabatic

/ ăd′ē-ə-bătĭk /

  1. Occurring without gain or loss of heat. When a gas is compressed under adiabatic conditions, its pressure increases and its temperature rises without the gain or loss of any heat. Conversely, when a gas expands under adiabatic conditions, its pressure and temperature both decrease without the gain or loss of heat. The adiabatic cooling of air as it rises in the atmosphere is the main cause of cloud formation.


Discover More

Other Words From

  • adi·a·bati·cal·ly adverb
Discover More

Word History and Origins

Origin of adiabatic1

1875–80; < Greek adiábat ( os ) incapable of being crossed ( a- a- 6 + dia- dia- + ba- (stem of baínein to cross) + -tos verbal adjective suffix) + -ic; diabatic
Discover More

Word History and Origins

Origin of adiabatic1

C19: from Greek adiabatos not to be crossed, impassable (to heat), from a- 1+ diabatos passable, from dia- across + bainein to go
Discover More

Example Sentences

At the same time the utmost pains are taken to maintain the adiabatic condition of the metal walls.

Adiabatic, ad-i-a-bat′ik, adj. (physics) neither losing nor gaining heat: impassable to heat.

This is the ratio of the adiabatic elasticity of air to the isothermal elasticity.

The adiabatic lines, representing a fall of temperature of 1° Fahrenheit per 183 feet of ascent, serve for comparison.

The straight dotted lines show the adiabatic decrease of temperature for ascending dry air.

Advertisement

Advertisement

Advertisement

Advertisement


adiabatadiabatic chart