Triple point explained

In thermodynamics, the triple point of a substance is the temperature and pressure at which the three phases (gas, liquid, and solid) of that substance coexist in thermodynamic equilibrium.[1] It is that temperature and pressure at which the sublimation, fusion, and vaporisation curves meet. For example, the triple point of mercury occurs at a temperature of NaN°C and a pressure of 0.165 mPa.

In addition to the triple point for solid, liquid, and gas phases, a triple point may involve more than one solid phase, for substances with multiple polymorphs. Helium-4 is unusual in that it has no sublimation/deposition curve and therefore no triple points where its solid phase meets its gas phase. Instead, it has a vapor-liquid-superfluid point, a solid-liquid-superfluid point, a solid-solid-liquid point, and a solid-solid-superfluid point. None of these should be confused with the Lambda Point, which is not any kind of triple point.

The term "triple point" was coined in 1873 by James Thomson, brother of Lord Kelvin.[2] The triple points of several substances are used to define points in the ITS-90 international temperature scale, ranging from the triple point of hydrogen (13.8033 K) to the triple point of water (273.16 K, 0.01 °C, or 32.018 °F).

Before 2019, the triple point of water was used to define the kelvin, the base unit of thermodynamic temperature in the International System of Units (SI).[3] The kelvin was defined so that the triple point of water is exactly 273.16 K, but that changed with the 2019 redefinition of SI base units, where the kelvin was redefined so that the Boltzmann constant is exactly 1.380649×10−23 J⋅K−1, and the triple point of water became an experimentally measured constant.

Triple point of water

Gas–liquid–solid triple point

Following the 2019 redefinition of the SI base units, the value of the triple point of water is no longer used as a defining point. However, its empirical value remains important: the unique combination of pressure and temperature at which liquid water, solid ice, and water vapor coexist in a stable equilibrium is approximately [4] and a vapor pressure of 611.657Pa.[5] [6]

Liquid water can only exist at pressures equal to or greater than the triple point. Below this, in the vacuum of outer space, solid ice sublimates, transitioning directly into water vapor when heated at a constant pressure. Conversely, above the triple point, solid ice first melts into liquid water upon heating at a constant pressure, then evaporates or boils to form vapor at a higher temperature.

For most substances, the gas–liquid–solid triple point is the minimum temperature where the liquid can exist. For water, this is not the case. The melting point of ordinary ice decreases with pressure, as shown by the phase diagram's dashed green line. Just below the triple point, compression at a constant temperature transforms water vapor first to solid and then to liquid.

Historically, during the Mariner 9 mission to Mars, the triple point pressure of water was used to define "sea level." Now, laser altimetry and gravitational measurements are preferred to define Martian elevation.[7]

High-pressure phases

At high pressures, water has a complex phase diagram with 15 known phases of ice and several triple points, including 10 whose coordinates are shown in the diagram. For example, the triple point at 251 K (−22 °C) and 210 MPa (2070 atm) corresponds to the conditions for the coexistence of ice Ih (ordinary ice), ice III and liquid water, all at equilibrium. There are also triple points for the coexistence of three solid phases, for example ice II, ice V and ice VI at 218 K (−55 °C) and 620 MPa (6120 atm).

For those high-pressure forms of ice which can exist in equilibrium with liquid, the diagram shows that melting points increase with pressure. At temperatures above 273 K (0 °C), increasing the pressure on water vapor results first in liquid water and then a high-pressure form of ice. In the range, ice I is formed first, followed by liquid water and then ice III or ice V, followed by other still denser high-pressure forms.

The various triple points of water! Phases in stable equilibrium! Pressure! Temperature
liquid water, ice Ih, and water vapor611.657 Pa[8] 273.16 K (0.01 °C)
liquid water, ice Ih, and ice III209.9 MPa251 K (−22 °C)
liquid water, ice III, and ice V350.1 MPa−17.0 °C
liquid water, ice V, and ice VI632.4 MPa0.16 °C
ice Ih, Ice II, and ice III213 MPa−35 °C
ice II, ice III, and ice V344 MPa−24 °C
ice II, ice V, and ice VI626 MPa−70 °C

Triple-point cells

Triple-point cells are used in the calibration of thermometers. For exacting work, triple-point cells are typically filled with a highly pure chemical substance such as hydrogen, argon, mercury, or water (depending on the desired temperature). The purity of these substances can be such that only one part in a million is a contaminant, called "six nines" because it is 99.9999% pure. A specific isotopic composition (for water, VSMOW) is used because variations in isotopic composition cause small changes in the triple point. Triple-point cells are so effective at achieving highly precise, reproducible temperatures, that an international calibration standard for thermometers called ITS–90 relies upon triple-point cells of hydrogen, neon, oxygen, argon, mercury, and water for delineating six of its defined temperature points.

Table of triple points

This table lists the gas–liquid–solid triple points of several substances. Unless otherwise noted, the data come from the U.S. National Bureau of Standards (now NIST, National Institute of Standards and Technology).[9]

Substance T [K] (°C) p [kPa]* (atm)
Acetylene192.4K 120abbr=onNaNabbr=on
Ammonia195.4K 6.06abbr=onNaNabbr=on
Argon83.8058K 68.9abbr=onNaNabbr=on
Arsenic1090K 3628abbr=onNaNabbr=on
Butane[10] 134.6K 0.0007abbr=onNaNabbr=on
Carbon (graphite)4765K 10132abbr=onNaNabbr=on
Carbon dioxide216.55K 517abbr=onNaNabbr=on
Carbon monoxide68.1K 15.37abbr=onNaNabbr=on
Chloroform[11] [12] 209.61K ?
Deuterium18.63K 17.1abbr=onNaNabbr=on
Ethane89.89K 0.0011abbr=onNaNabbr=on
Ethanol[13] 150K 4.3E-07abbr=onNaNabbr=on
Ethylene104K 0.12abbr=onNaNabbr=on
Formic acid[14] 281.4K 2.2abbr=onNaNabbr=on
Helium-4 (vapor−He-I−He-II)[15] 2.1768K 5.048abbr=onNaNabbr=on
Helium-4 (hcpbcc−He-II)[16] 1.463K 26.036abbr=onNaNabbr=on
Helium-4 (bcc−He-I−He-II)1.762K 29.725abbr=onNaNabbr=on
Helium-4 (hcp−bcc−He-I)1.772K 30.016abbr=onNaNabbr=on
Hexafluoroethane[17] 173.08K 26.6abbr=onNaNabbr=on
Hydrogen13.8033K 7.04abbr=onNaNabbr=on
Hydrogen-1 (Protium)[18] 13.96K 7.18abbr=onNaNabbr=on
Hydrogen chloride158.96K 13.9abbr=onNaNabbr=on
Iodine[19] 386.65K 12.07abbr=onNaNabbr=on
Isobutane[20] 113.55K 1.9481E-05abbr=onNaNabbr=on
Krypton115.76K 74.12abbr=onNaNabbr=on
Mercury234.3156K 1.65E-07abbr=onNaNabbr=on
Methane90.68K 11.7abbr=onNaNabbr=on
Neon24.5561K 43.332abbr=onNaNabbr=on
Nitric oxide109.5K 21.92abbr=onNaNabbr=on
Nitrogen63.18K 12.6abbr=onNaNabbr=on
Nitrous oxide182.34K 87.85abbr=onNaNabbr=on
Oxygen54.3584K 0.14625abbr=onNaNabbr=on
Palladium1825K 0.0035abbr=onNaNabbr=on
Platinum2045K 0.0002abbr=onNaNabbr=on
Radon202K 70abbr=onNaNabbr=on
(mono)Silane[21] 88.48K 0.019644abbr=onNaNabbr=on
Sulfur dioxide197.69K 1.67abbr=onNaNabbr=on
Titanium1941K 0.0053abbr=onNaNabbr=on
Uranium hexafluoride337.17K 151.7abbr=onNaNabbr=on
Water273.16K 0.611657abbr=onNaNabbr=on
Xenon161.3K 81.5abbr=onNaNabbr=on
Zinc692.65K 0.065abbr=onNaNabbr=on
Notes:

See also

Notes and References

  1. .
  2. James Thomson (1873) "A quantitative investigation of certain relations between the gaseous, the liquid, and the solid states of water-substance", Proceedings of the Royal Society, 22 : 27–36. From a footnote on page 28: " … the three curves would meet or cross each other in one point, which I have called the triple point".
  3. http://www1.bipm.org/en/si/base_units/ Definition of the kelvin
  4. Web site: SI Brochure: The International System of Units (SI) – 9th edition . BIPM . 21 February 2022.
  5. https://www.nist.gov/srd/upload/jpcrd477.pdf International Equations for the Pressure along the Melting and along the Sublimation Curve of Ordinary Water Substance
  6. 10.1256/qj.04.94 . 131 . 608 . Review of the vapour pressures of ice and supercooled water for atmospheric applications . 2005 . Quarterly Journal of the Royal Meteorological Society . 1539–1565 . Murphy . D. M.. 2005QJRMS.131.1539M. 122365938 . free .
  7. Book: Carr, Michael H. . The Surface of Mars . limited . Cambridge University Press . 2007 . 5 . 978-0-521-87201-0 .
  8. 10.1256/qj.04.94 . 131 . 608 . Review of the vapour pressures of ice and supercooled water for atmospheric applications . 2005 . Quarterly Journal of the Royal Meteorological Society . 1539–1565 . Murphy . D. M.. 2005QJRMS.131.1539M . 122365938 . free .
  9. Book: Yunus A. . Cengel . Robert H. . Turner . Fundamentals of thermal-fluid sciences . Boston . McGraw-Hill . 2004 . 78 . 0-07-297675-6 .
  10. See Butane (data page)
  11. See Chloroform (data page)
  12. Web site: Trichloromethane . NIST Chemistry WebBook, SRD 69 . NIST (National Institute of Science and Technology) . 11 May 2024.
  13. See Ethanol (data page)
  14. See Formic acid (data page)
  15. The Observed Properties of Liquid Helium at the Saturated Vapor Pressure . Russell J.. Donnelly. Carlo F.. Barenghi. Journal of Physical and Chemical Reference Data. 1998. 27. 6. 1217–1274. 10.1063/1.556028. 1998JPCRD..27.1217D .
  16. Thermodynamic properties of 4He. II. The bcc phase and the P-T and VT phase diagrams below 2 K . J. K.. Hoffer. W. R.. Gardner. C. G.. Waterfield. N. E.. Phillips. Journal of Low Temperature Physics. April 1976. 23. 1. 63–102. 10.1007/BF00117245. 1976JLTP...23...63H . 120473493.
  17. See Hexafluoroethane (data page)
  18. Web site: Protium | isotope | Britannica . 27 January 2024 .
  19. Book: Walas, S. M. . Chemical Process Equipment – Selection and Design . Amsterdam . Elsevier . 1990 . 639 . 0-7506-7510-1 .
  20. See Isobutane (data page)
  21. Web site: Silane-Gas Encyclopedia . . Gas Encyclopedia . Air Liquide . automatically using date of last page refresh makes no sense for a citation --> .