freezing point

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(frē'zĭng)
n. (Abbr. fp)
  1. The temperature at which a liquid of specified composition solidifies under a specified pressure.
  2. The temperature at which the liquid and solid phases of a substance of specified composition are in equilibrium at atmospheric pressure.


Temperature at which a liquid becomes a solid. When the pressure surrounding the liquid is increased, the freezing point is raised. The addition of some solids can lower the freezing point of a liquid, a principle used when salt is applied to melt ice on frozen surfaces. For pure substances, the freezing point is the same as the melting point. In mixtures and certain organic compounds, the early solid formation changes the composition of the remaining liquid, usually steadily lowering its freezing point, a principle that is applied in mixture separation. The freezing point of pure water at standard atmospheric pressure is 32F (0C). To change a liquid at its freezing point to a solid at the same temperature, the heat of fusion ( latent heat) must be removed.

For more information on freezing point, visit Britannica.com.

The temperature at which a liquid changes into a solid; the same temperature as the melting point. (See phases of matter.)

  • Water freezes at thirty-two degrees Fahrenheit or zero degrees Celsius.
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    The temperature at which a liquid turns into a solid.

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    fp (abbreviation)
    cryoscope (engineering)
    ice line (thermodynamics)
    freezing mixture (physical chemistry)