In
thermochemistry,
latent heat is the amount of
energy in the form of
heat released or absorbed by a substance during a change of
phase (for example solid, liquid, or gas), - also called a phase transition.
The term was introduced around
1750 by
Joseph Black as derived from the Latin
latere, to lie hidden. The term is now obsolete, replaced by "
enthalpy of transformation".
Two latent heats (or enthalpies) are typically described: latent
heat of fusion (
melting), and latent
heat of vaporization (
boiling). The names describe the direction of heat flow from one phase to the next: solid → liquid → gas.
The change is
endothermic, for example the system absorbs energy, when the change is from solid to liquid to gas. It is
exothermic (the process releases energy) when it's in the opposite direction. For example, in the
atmosphere, when a molecule of
water evaporates from the surface of any body of water,
energy is transported by the water molecule into a lower temperature
air parcel that contains more
water vapor than its surroundings. Because energy is needed to overcome the molecular forces of attraction between water particles, the process of transition from a parcel of water to a parcel of vapor requires the input of energy causing a drop in temperature in its surroundings. If the water vapor condenses back to a liquid or solid
phase onto a surface, the latent energy absorbed during evaporation is released as
sensible heat onto the surface. The large value of the enthalpy of condensation of water vapor is the reason that steam is a far more effective heating medium than boiling water, and is more hazardous.
Latent Heat Equation
The equation for latent heat is:
Q = mL
where:
Q is the amount of energy required to change the phase of the substance,
m is the mass of the substance,
L is the specific latent heat for a particular substance.
In other words, specific latent heat is found when energy is divided by mass.
Table of latent heats
External results
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