:''For freezing as a method of food preservation, see
frozen food.''
In
physics and
chemistry, 'freezing' is the process whereby a
liquid turns to a
solid. The
freezing point is the
temperature at which this happens.
Melting, the process of turning a solid to a liquid, is the opposite of freezing. For most substances, the melting and freezing points are the same temperature.
Rapid cooling by exposure to
cryogenic temperatures can cause a substance to freeze below its melting point, a process known as
flash freezing. For some pure substances, such as
pure water, the freezing temperature is lower than the melting temperature. The freezing point for water is only the same temperature as the
melting point when
nucleators are present to prevent
supercooling. The freezing point of water is 0°C (32°F, 273 K). In the absence of nucleators water will supercool to as low as −70°C (−94°F, 203 K) before freezing.
[1] But in the presence of nucleating substances the freezing point of water is the same as the melting point. Nucleating agents, such as dust, are commonly present in the environment, which is why
rain water and
tap water will normally freeze at the melting point of water.
Food preservation
Main articles: Frozen food
Freezing is a common method of
food preservation which slows both food decay and the growth of
micro-organisms. Besides the effect of lower temperatures on
reaction rates, freezing makes water less available for
bacterial growth. there are many forms of freezing see below for details
References
1.
See also
★
Flash freezing
★
Nucleation
★
Supercooling
★
Melting point
★
Frost
External links
★
Freezing of water, an enigma
: