Phases of fluorine

Fluorine forms diatomic molecules (F
2
) that are gaseous at room temperature with a density about 1.3 times that of air.[1][note 1] Though sometimes cited as yellow-green, pure fluorine gas is actually a very pale yellow. The color can only be observed in concentrated fluorine gas when looking down the axis of long tubes, as it appears transparent when observed from the side in normal tubes or if allowed to escape into the atmosphere.[3] The element has a "pungent" characteristic odor that is noticeable in concentrations as low as 20 ppb.[4]

Fluorine condenses to a bright yellow liquid at −188 °C (−307 °F),[5] which is near the condensation temperatures of oxygen and nitrogen.

The solid state of fluorine relies on Van der Waals forces to hold molecules together, which, because of the small size of the fluorine molecules, are relatively weak. Consequently, the solid state of fluorine is more similar to that of oxygen[6][7] or the noble gases than to those of the heavier halogens.

Fluorine solidifies at −220 °C (−363 °F)[5] into a cubic structure, called beta-fluorine. This phase is transparent and soft, with significant disorder of the molecules; its density is 1.70 g/cm3. At −228 °C (−378 °F) fluorine undergoes a solid–solid phase transition into a monoclinic structure called alpha-fluorine.

This phase is opaque and hard, with close-packed layers of molecules, and is denser at 1.97 g/cm3.[9] The solid state phase change requires more energy than the melting point transition and can be violent, shattering samples and blowing out sample holder windows.[10][11]

History

Henri Moissan was the first to isolate the element in 1886, observing its gaseous phase. Eleven years later, Sir James Dewar first liquified the element. For unclear reasons, Dewar measured a density for the liquid about 40% too small, and would not be corrected until 1951.[12]:4,110 Solid fluorine received significant study in the 1920s and 30s, but relatively less until the 1960s. The crystal structure of alpha-fluorine given, which still has some uncertainty, dates to a 1970 paper by Linus Pauling.

Notes

  1. Density of air at 100 kilopascal and 0 °C is 1.2724 g/L.[2]

Citations

  1. Jaccaud et al. 2005, p. 2.
  2. Shelquist, Richard (2010). "An introduction to air density and density altitude calculations". Shelquist Engineering. Retrieved 29 April 2011.
  3. Burdon, Emson & Edwards 1987, p. 471.
  4. Lide 2004, p. 4.12.
  5. Dean 1999, p. 523.
  6. Jordan, Streib & Lipscomb 1964, p. 760.
  7. Jordan et al. 1964.
  8. Jordan, Streib & Lipscomb 1964, Fig. 1
  9. Meyer, Barrett & Greer 1969.
  10. Young 1975, p. 10
  11. Barrett, Meyer & Wasserman 1967.
  12. Clark, John Drury (23 May 2018). Ignition!: An Informal History of Liquid Rocket Propellants. Rutgers University Press. p. 302. ISBN 978-0-8135-9918-2. OCLC 281664.

Indexed references

Further reading

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.