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   » » Wiki: Allotropes Of Oxygen
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There are several known of . The most familiar is (), present at significant levels in Earth's atmosphere and also known as dioxygen or . Another is the highly reactive (). Others are:


Atomic oxygen
Atomic oxygen, denoted O or O1, is very reactive, as the individual atoms of oxygen tend to quickly bond with nearby molecules. Its lowest-energy electronic state is a , designated by the 3P. On Earth's surface, it exists naturally for a very short time. In , the presence of ample ultraviolet radiation results in a low Earth orbit atmosphere in which 96% of the oxygen occurs in atomic form. "Out of Thin Air" .NASA.gov. February 17, 2011.

Atomic oxygen has been detected on by , , and the SOFIA observatory.


Dioxygen
The common allotrope of elemental oxygen on Earth, , is generally known as oxygen, but may be called dioxygen, diatomic oxygen, molecular oxygen, dioxidene or oxygen gas to distinguish it from the element itself and from the triatomic allotrope , . As a major component (about 21% by volume) of Earth's atmosphere, elemental oxygen is most commonly encountered in the diatomic form. use atmospheric dioxygen as the terminal oxidant in cellular respiration in order to obtain . The of dioxygen is known as , , because it has two unpaired electrons. The first excited state, , , has no unpaired electrons and is . The state requires an odd number of electrons, and so cannot occur in dioxygen without gaining or losing electrons, such as in the ion () or the ion ().

The ground state of has a bond length of 121  and a bond energy of 498 kJ/mol. It is a colourless gas with a boiling point of . It can be condensed from air by cooling with , which has a boiling point of . Liquid oxygen is pale blue in colour, and is quite markedly due to the unpaired electrons; liquid oxygen contained in a flask suspended by a string is attracted to a magnet.


Singlet oxygen
is the common name used for the two of molecular () with higher energy than the ground state . Because of the differences in their electron shells, singlet oxygen has different chemical and physical properties than triplet oxygen, including absorbing and emitting light at different wavelengths. It can be generated in a photosensitized process by energy transfer from dye molecules such as , or , or by chemical processes such as spontaneous decomposition of in water or the reaction of hydrogen peroxide with .


Ozone
Triatomic oxygen (ozone, ) is a very reactive allotrope of oxygen that is a pale blue gas at standard temperature and pressure. Liquid and solid have a deeper blue color than ordinary , and they are unstable and explosive.Mellor 1939Cotton, F. Albert and Wilkinson, Geoffrey (1972). Advanced Inorganic Chemistry: A comprehensive Text. (3rd Edition). New York, London, Sydney, Toronto: Interscience Publications. . In its gas phase, ozone is destructive to materials like and and is damaging to tissue.Stwertka 1998, p.48 Traces of it can be detected as a pungent, chlorine-like smell, Chemistry Tutorial : Allotropes from AUS-e-TUTE.com.au coming from , , and , as it is formed whenever air is subjected to an electrical discharge. It was named "ozon" in 1840 by Christian Friedrich Schönbein,Christian Friedrich Schönbein, Über die Erzeugung des Ozons auf chemischen Wege , p. 3, Basel: Schweighauser'sche Buchhandlung, 1844. from ancient Greek ὄζειν (ozein: "to smell") plus the suffix -on, commonly used at the time to designate a derived compound and anglicized as -one."Ozone", Oxford English Dictionary online, retrieved 29 June 2020.

Ozone is thermodynamically unstable and tends to react toward the more common dioxygen form. It is formed by reaction of intact with atomic oxygen produced when in the splits . Ozone absorbs strongly in the ultraviolet and in the stratosphere functions as a shield for the against and other damaging effects of (see ). Tropospheric ozone is formed near the Earth's surface by the photochemical disintegration of in the exhaust of .Stwertka 1998, p.49 Ground-level ozone is an that is especially harmful for senior citizens (elderly), children, and people with heart and lung conditions such as , , and . The produces ozone as an antimicrobial (see below).


Cyclic ozone
Cyclic ozone is a theoretically predicted molecule in which its three atoms of oxygen bond in an equilateral triangle instead of an open angle.


Tetraoxygen
Tetraoxygen had been suspected to exist since the early 1900s, when it was known as oxozone. It was identified in 2001 by a team led by Fulvio Cacace at the University of Rome. The molecule was thought to be in one of the phases of later identified as . Cacace's team suggested that probably consists of two dumbbell-like molecules loosely held together by induced dipole dispersion forces.


Phases of solid oxygen
There are six known distinct phases of solid oxygen. One of them is a dark-red cluster. When oxygen is subjected to a pressure of 96 GPa, it becomes , in a similar manner to , and becomes more similar to the heavier , such as (exhibiting a pink-red color in its elemental state), and , both of which show significant metallic character. At very low temperatures, this phase also becomes .


Further reading
  • Theoretical analysis of some and lead-ref for others:

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