Difference between revisions of "Isothermal Equilibrium"
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Isothermal Equilibrium
</dt>
The state of an atmosphere
at rest, uninfluenced by any external agency, in which the conduction of heat
from one part to another has, after a sufficient length of time, produced a
uniform temperature throughout its entire mass. Also called conductive
equilibrium. See diffusive
equilibrium, isothermal
atmosphere. [[/a>|/a>
]]
References
This article is based on NASA's Dictionary of Technical Terms for Aerospace Use
