Evaporability

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The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.

Evaporability

 

an arbitrary quantity that characterizes the potentially possible evaporation (evaporation not restricted by the water supply) in a given area under existing atmospheric conditions. It is measured with an atmometer from the surface of the water or from the surface of a large natural basin of fresh water or supersaturated soil. Evaporability is expressed in millimeters of the layer of water evaporated. For example, the average annual evaporability in Leningrad is 320 mm; in Moscow, 417 mm; in Odessa, 584 mm; and in Nukus (Middle Asia), 1,718 mm.

Evaporability can differ greatly from the actual evaporation from the surface of the soil and from plants, especially in an arid desert, where actual evaporation is close to zero because of the complete absence of water, but where evaporability reaches 2,000 mm a year and more.

The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.
References in periodicals archive ?
Evaporable getters are often used in electron tubes where a mirror-like metal coating can be easily observed on the inside of the glass envelope.
In the study of Han [12], modified chloride diffusion coefficient was proposed as a function of chloride binding, evaporable water content, and diffusion coefficient.
In the FAGC samples, an endothermic peak was observed between 50[degrees]C and 70[degrees]C, which was attributed to the loss of evaporable water in the sample, and the water was combined in the aluminosilicates [30].
This adsorption thus increases the amount of evaporable water.
Getters are classified as being either evaporable or nonevaporable.