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heat of sublimation

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heat of sublimation [′hēt əv ‚səb·lə′mā·shən]
(thermodynamics)
The increase in enthalpy accompanying the conversion of 1 mole, or unit mass, of a solid to a vapor at constant pressure and temperature. Also known as latent heat of sublimation.


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CO2 is the most effective dry cooling agent because it forms snow with a high latent heat of sublimation at -78 degrees C.
 
 
 
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