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Freezing

Freezing is a phase transition where a liquid turns into a solid when its temperature is lowered below its freezing point. In accordance with the internationally established definition, freezing means the solidification phase change of a liquid or the liquid content of a substance, usually due to cooling.[1][2]

Water dripping from a slab of ice and then freezing, forming icicles

For most substances, the melting and freezing points are the same temperature; however, certain substances possess differing solid-liquid transition temperatures. For example, agar displays a hysteresis in its melting point and freezing point. It melts at 85 °C (185 °F) and solidifies from 32 °C to 40 °C (89.6 °F to 104 °F).[3]

Crystallization edit

Most liquids freeze by crystallization, formation of crystalline solid from the uniform liquid. This is a first-order thermodynamic phase transition, which means that as long as solid and liquid coexist, the temperature of the whole system remains very nearly equal to the melting point due to the slow removal of heat when in contact with air, which is a poor heat conductor.[citation needed] Because of the latent heat of fusion, the freezing is greatly slowed and the temperature will not drop anymore once the freezing starts but will continue dropping once it finishes.[citation needed]

Crystallization consists of two major events, nucleation and crystal growth. "Nucleation" is the step wherein the molecules start to gather into clusters, on the nanometer scale, arranging in a defined and periodic manner that defines the crystal structure. "Crystal growth" is the subsequent growth of the nuclei that succeed in achieving the critical cluster size. The thermodynamics of freezing and melting is a classical discipline within physical chemistry,[4] which nowadays develops in conjunction with computer simulations.[5]

Supercooling edit

Rapid formation of ice crystals in supercool water (home freezer experiment)

In spite of the second law of thermodynamics, crystallization of pure liquids usually begins at a lower temperature than the melting point, due to high activation energy of homogeneous nucleation. The creation of a nucleus implies the formation of an interface at the boundaries of the new phase. Some energy is expended to form this interface, based on the surface energy of each phase. If a hypothetical nucleus is too small, the energy that would be released by forming its volume is not enough to create its surface, and nucleation does not proceed. Freezing does not start until the temperature is low enough to provide enough energy to form stable nuclei. In presence of irregularities on the surface of the containing vessel, solid or gaseous impurities, pre-formed solid crystals, or other nucleators, heterogeneous nucleation may occur, where some energy is released by the partial destruction of the previous interface, raising the supercooling point to be near or equal to the melting point. The melting point of water at 1 atmosphere of pressure is very close to 0 °C (32 °F, 273.15 K), and in the presence of nucleating substances the freezing point of water is close to the melting point, but in the absence of nucleators water can supercool to −40 °C (−40 °F; 233 K) before freezing. [6][7] Under high pressure (2,000 atmospheres) water will supercool to as low as −70 °C (−94 °F; 203 K) before freezing. [8]

Exothermicity edit

Freezing is almost always an exothermic process, meaning that as liquid changes into solid, heat and pressure are released. This is often seen as counter-intuitive,[9] since the temperature of the material does not rise during freezing, except if the liquid were supercooled. But this can be understood since heat must be continually removed from the freezing liquid or the freezing process will stop. The energy released upon freezing is a latent heat, and is known as the enthalpy of fusion and is exactly the same as the energy required to melt the same amount of the solid.

Low-temperature helium is the only known exception to the general rule.[10] Helium-3 has a negative enthalpy of fusion at temperatures below 0.3 K. Helium-4 also has a very slightly negative enthalpy of fusion below 0.8 K. This means that, at appropriate constant pressures, heat must be added to these substances in order to freeze them.[11]

Vitrification edit

Certain materials, such as glass and glycerol, may harden without crystallizing; these are called amorphous solids. Amorphous materials, as well as some polymers, do not have a freezing point, as there is no abrupt phase change at any specific temperature. Instead, there is a gradual change in their viscoelastic properties over a range of temperatures. Such materials are characterized by a glass transition that occurs at a glass transition temperature, which may be roughly defined as the "knee" point of the material's density vs. temperature graph. Because vitrification is a non-equilibrium process, it does not qualify as freezing, which requires an equilibrium between the crystalline and liquid state.

Expansion edit

The size of substances increases or expands on being heated. This increase in the size of a body due to heating is called thermal expansion .. Thermal expansion takes place in all objects and in all states of matter. However different substances have different rates of expansion for the same rise in temperature.

Freezing of living organisms edit

Many living organisms are able to tolerate prolonged periods of time at temperatures below the freezing point of water. Most living organisms accumulate cryoprotectants such as anti-nucleating proteins, polyols, and glucose to protect themselves against frost damage by sharp ice crystals. Most plants, in particular, can safely reach temperatures of −4 °C to −12 °C. Certain bacteria, notably Pseudomonas syringae, produce specialized proteins that serve as potent ice nucleators, which they use to force ice formation on the surface of various fruits and plants at about −2 °C.[12] The freezing causes injuries in the epithelia and makes the nutrients in the underlying plant tissues available to the bacteria.[13]

Bacteria edit

Three species of bacteria, Carnobacterium pleistocenium, as well as Chryseobacterium greenlandensis and Herminiimonas glaciei, have reportedly been revived after surviving for thousands of years frozen in ice.

Plants edit

Many plants undergo a process called hardening, which allows them to survive temperatures below 0 °C for weeks to months.

Animals edit

The nematode Haemonchus contortus can survive 44 weeks frozen at liquid nitrogen temperatures. Other nematodes that survive at temperatures below 0 °C include Trichostrongylus colubriformis and Panagrolaimus davidi. Many species of reptiles and amphibians survive freezing.

Human gametes and 2-, 4- and 8-cell embryos can survive freezing and are viable for up to 10 years, a process known as cryopreservation.

Experimental attempts to freeze human beings for later revival are known as cryonics.

Food preservation edit

Freezing is a common method of food preservation that 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 bacteria growth. freezing is one of the oldest and most widely used method of food preservation as far back as 1842, freezing has been immensely used in an ice and salt brine. In freezing, flavours, smell and nutritional content most generally remain unchanged. Freezing became commercially applicable after the advent (introduction) of mechanical refrigeration. Freezing has been successfully employed for long term preservation of many foods providing a significantly extended shelf-life. Freezing preservation is generally regarded as superior to canning and dehydration with respect to retention in sensory attributes and nutritive attributes.

See also edit

Table edit

Phase transitions of matter ()
To
From
Solid Liquid Gas Plasma
Solid Melting Sublimation
Liquid Freezing Vaporization
Gas Deposition Condensation Ionization
Plasma Recombination

References edit

  1. ^ . International Dictionary of Refrigeration. Archived from the original on 2019-10-01. Retrieved 2022-11-03.
  2. ^ "freezing". ASHRAE Terminology. Retrieved 2022-11-03. — via https://www.ashrae.org/technical-resources/free-resources/ashrae-terminology
  3. ^ . Sciencebuddies.org. Archived from the original on 2011-06-03. Retrieved 2011-04-27.
  4. ^ Atkins PW (2017). Elements of physical chemistry. Oxford University Press. ISBN 978-0-19-879670-1. OCLC 982685277.
  5. ^ Pedersen UR, Costigliola L, Bailey NP, Schrøder TB, Dyre JC (August 2016). "Thermodynamics of freezing and melting". Nature Communications. 7 (1): 12386. Bibcode:2016NatCo...712386P. doi:10.1038/ncomms12386. PMC 4992064. PMID 27530064.
  6. ^ Lundheim R (July 2002). "Physiological and ecological significance of biological ice nucleators". Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences. 357 (1423): 937–43. doi:10.1098/rstb.2002.1082. PMC 1693005. PMID 12171657.
  7. ^ Franks F (March 2003). "Nucleation of ice and its management in ecosystems" (PDF). Philosophical Transactions. Series A, Mathematical, Physical, and Engineering Sciences. 361 (1804): 557–74, discussion 574. Bibcode:2003RSPTA.361..557F. doi:10.1098/rsta.2002.1141. PMID 12662454. S2CID 25606767.
  8. ^ Jeffery CA, Austin PH (November 1997). "Homogeneous nucleation of supercooled water: Results from a new equation of state". Journal of Geophysical Research. 102 (D21): 25269–25280. Bibcode:1997JGR...10225269J. CiteSeerX 10.1.1.9.3236. doi:10.1029/97JD02243.
  9. ^ What is an exothermic reaction? Scientific American, 1999
  10. ^ Atkins P, Jones L (2008), Chemical Principles: The Quest for Insight (4th ed.), W. H. Freeman and Company, p. 236, ISBN 978-0-7167-7355-9
  11. ^ Ott JB, Boerio-Goates J (2000). Chemical Thermodynamics: Advanced Applications. Academic Press. pp. 92–93. ISBN 0-12-530985-6.
  12. ^ Maki LR, Galyan EL, Chang-Chien MM, Caldwell DR (September 1974). "Ice nucleation induced by pseudomonas syringae". Applied Microbiology. 28 (3): 456–9. doi:10.1128/aem.28.3.456-459.1974. PMC 186742. PMID 4371331.
  13. ^ Zachariassen KE, Kristiansen E (December 2000). "Ice nucleation and antinucleation in nature". Cryobiology. 41 (4): 257–79. doi:10.1006/cryo.2000.2289. PMID 11222024.

External links edit

  •   Media related to Freezing at Wikimedia Commons
  • Video of an intermetallic compound solidifying/freezing 2015-12-10 at the Wayback Machine

freezing, other, uses, disambiguation, phase, transition, where, liquid, turns, into, solid, when, temperature, lowered, below, freezing, point, accordance, with, internationally, established, definition, freezing, means, solidification, phase, change, liquid,. For other uses see Freezing disambiguation Freezing is a phase transition where a liquid turns into a solid when its temperature is lowered below its freezing point In accordance with the internationally established definition freezing means the solidification phase change of a liquid or the liquid content of a substance usually due to cooling 1 2 Water dripping from a slab of ice and then freezing forming iciclesFor most substances the melting and freezing points are the same temperature however certain substances possess differing solid liquid transition temperatures For example agar displays a hysteresis in its melting point and freezing point It melts at 85 C 185 F and solidifies from 32 C to 40 C 89 6 F to 104 F 3 Contents 1 Crystallization 2 Supercooling 3 Exothermicity 4 Vitrification 5 Expansion 6 Freezing of living organisms 6 1 Bacteria 6 2 Plants 6 3 Animals 7 Food preservation 8 See also 9 Table 10 References 11 External linksCrystallization editMain article Crystallization Most liquids freeze by crystallization formation of crystalline solid from the uniform liquid This is a first order thermodynamic phase transition which means that as long as solid and liquid coexist the temperature of the whole system remains very nearly equal to the melting point due to the slow removal of heat when in contact with air which is a poor heat conductor citation needed Because of the latent heat of fusion the freezing is greatly slowed and the temperature will not drop anymore once the freezing starts but will continue dropping once it finishes citation needed Crystallization consists of two major events nucleation and crystal growth Nucleation is the step wherein the molecules start to gather into clusters on the nanometer scale arranging in a defined and periodic manner that defines the crystal structure Crystal growth is the subsequent growth of the nuclei that succeed in achieving the critical cluster size The thermodynamics of freezing and melting is a classical discipline within physical chemistry 4 which nowadays develops in conjunction with computer simulations 5 Supercooling editMain article Supercooling source source Rapid formation of ice crystals in supercool water home freezer experiment In spite of the second law of thermodynamics crystallization of pure liquids usually begins at a lower temperature than the melting point due to high activation energy of homogeneous nucleation The creation of a nucleus implies the formation of an interface at the boundaries of the new phase Some energy is expended to form this interface based on the surface energy of each phase If a hypothetical nucleus is too small the energy that would be released by forming its volume is not enough to create its surface and nucleation does not proceed Freezing does not start until the temperature is low enough to provide enough energy to form stable nuclei In presence of irregularities on the surface of the containing vessel solid or gaseous impurities pre formed solid crystals or other nucleators heterogeneous nucleation may occur where some energy is released by the partial destruction of the previous interface raising the supercooling point to be near or equal to the melting point The melting point of water at 1 atmosphere of pressure is very close to 0 C 32 F 273 15 K and in the presence of nucleating substances the freezing point of water is close to the melting point but in the absence of nucleators water can supercool to 40 C 40 F 233 K before freezing 6 7 Under high pressure 2 000 atmospheres water will supercool to as low as 70 C 94 F 203 K before freezing 8 Exothermicity editMain article Enthalpy of fusion Freezing is almost always an exothermic process meaning that as liquid changes into solid heat and pressure are released This is often seen as counter intuitive 9 since the temperature of the material does not rise during freezing except if the liquid were supercooled But this can be understood since heat must be continually removed from the freezing liquid or the freezing process will stop The energy released upon freezing is a latent heat and is known as the enthalpy of fusion and is exactly the same as the energy required to melt the same amount of the solid Low temperature helium is the only known exception to the general rule 10 Helium 3 has a negative enthalpy of fusion at temperatures below 0 3 K Helium 4 also has a very slightly negative enthalpy of fusion below 0 8 K This means that at appropriate constant pressures heat must be added to these substances in order to freeze them 11 Vitrification editMain article Glass transition Certain materials such as glass and glycerol may harden without crystallizing these are called amorphous solids Amorphous materials as well as some polymers do not have a freezing point as there is no abrupt phase change at any specific temperature Instead there is a gradual change in their viscoelastic properties over a range of temperatures Such materials are characterized by a glass transition that occurs at a glass transition temperature which may be roughly defined as the knee point of the material s density vs temperature graph Because vitrification is a non equilibrium process it does not qualify as freezing which requires an equilibrium between the crystalline and liquid state Expansion editThe size of substances increases or expands on being heated This increase in the size of a body due to heating is called thermal expansion Thermal expansion takes place in all objects and in all states of matter However different substances have different rates of expansion for the same rise in temperature Freezing of living organisms editMain article Cryobiology Many living organisms are able to tolerate prolonged periods of time at temperatures below the freezing point of water Most living organisms accumulate cryoprotectants such as anti nucleating proteins polyols and glucose to protect themselves against frost damage by sharp ice crystals Most plants in particular can safely reach temperatures of 4 C to 12 C Certain bacteria notably Pseudomonas syringae produce specialized proteins that serve as potent ice nucleators which they use to force ice formation on the surface of various fruits and plants at about 2 C 12 The freezing causes injuries in the epithelia and makes the nutrients in the underlying plant tissues available to the bacteria 13 Bacteria edit Three species of bacteria Carnobacterium pleistocenium as well as Chryseobacterium greenlandensis and Herminiimonas glaciei have reportedly been revived after surviving for thousands of years frozen in ice Plants edit Many plants undergo a process called hardening which allows them to survive temperatures below 0 C for weeks to months Animals edit The nematode Haemonchus contortus can survive 44 weeks frozen at liquid nitrogen temperatures Other nematodes that survive at temperatures below 0 C include Trichostrongylus colubriformis and Panagrolaimus davidi Many species of reptiles and amphibians survive freezing Human gametes and 2 4 and 8 cell embryos can survive freezing and are viable for up to 10 years a process known as cryopreservation Experimental attempts to freeze human beings for later revival are known as cryonics Food preservation editMain article Frozen food Freezing is a common method of food preservation that 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 bacteria growth freezing is one of the oldest and most widely used method of food preservation as far back as 1842 freezing has been immensely used in an ice and salt brine In freezing flavours smell and nutritional content most generally remain unchanged Freezing became commercially applicable after the advent introduction of mechanical refrigeration Freezing has been successfully employed for long term preservation of many foods providing a significantly extended shelf life Freezing preservation is generally regarded as superior to canning and dehydration with respect to retention in sensory attributes and nutritive attributes See also editDegree of frost Directional freezing Flash freezing Fractional freezing Freezer Freezing air temperature Frost Micro pulling down Mpemba effect Phase diagramTable editPhase transitions of matter vte ToFrom Solid Liquid Gas PlasmaSolid Melting SublimationLiquid Freezing VaporizationGas Deposition Condensation IonizationPlasma RecombinationReferences edit freezing International Dictionary of Refrigeration Archived from the original on 2019 10 01 Retrieved 2022 11 03 freezing ASHRAE Terminology Retrieved 2022 11 03 via https www ashrae org technical resources free resources ashrae terminology All About Agar Sciencebuddies org Archived from the original on 2011 06 03 Retrieved 2011 04 27 Atkins PW 2017 Elements of physical chemistry Oxford University Press ISBN 978 0 19 879670 1 OCLC 982685277 Pedersen UR Costigliola L Bailey NP Schroder TB Dyre JC August 2016 Thermodynamics of freezing and melting Nature Communications 7 1 12386 Bibcode 2016NatCo 712386P doi 10 1038 ncomms12386 PMC 4992064 PMID 27530064 Lundheim R July 2002 Physiological and ecological significance of biological ice nucleators Philosophical Transactions of the Royal Society of London Series B Biological Sciences 357 1423 937 43 doi 10 1098 rstb 2002 1082 PMC 1693005 PMID 12171657 Franks F March 2003 Nucleation of ice and its management in ecosystems PDF Philosophical Transactions Series A Mathematical Physical and Engineering Sciences 361 1804 557 74 discussion 574 Bibcode 2003RSPTA 361 557F doi 10 1098 rsta 2002 1141 PMID 12662454 S2CID 25606767 Jeffery CA Austin PH November 1997 Homogeneous nucleation of supercooled water Results from a new equation of state Journal of Geophysical Research 102 D21 25269 25280 Bibcode 1997JGR 10225269J CiteSeerX 10 1 1 9 3236 doi 10 1029 97JD02243 What is an exothermic reaction Scientific American 1999 Atkins P Jones L 2008 Chemical Principles The Quest for Insight 4th ed W H Freeman and Company p 236 ISBN 978 0 7167 7355 9 Ott JB Boerio Goates J 2000 Chemical Thermodynamics Advanced Applications Academic Press pp 92 93 ISBN 0 12 530985 6 Maki LR Galyan EL Chang Chien MM Caldwell DR September 1974 Ice nucleation induced by pseudomonas syringae Applied Microbiology 28 3 456 9 doi 10 1128 aem 28 3 456 459 1974 PMC 186742 PMID 4371331 Zachariassen KE Kristiansen E December 2000 Ice nucleation and antinucleation in nature Cryobiology 41 4 257 79 doi 10 1006 cryo 2000 2289 PMID 11222024 External links edit nbsp Look up freezing in Wiktionary the free dictionary nbsp Media related to Freezing at Wikimedia Commons Video of an intermetallic compound solidifying freezing Archived 2015 12 10 at the Wayback Machine Retrieved from https en wikipedia org w index php title Freezing amp oldid 1185730300, wikipedia, wiki, book, books, library,

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