Iodine dioxide: Difference between revisions
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'''Iodine dioxide''' is a binary [[inorganic compound]] of [[iodine]] and [[oxygen]] with the chemical formula {{chem|I|O|2}}.<ref>{{cite book |last1=Yaws |first1=Carl |title=The Yaws Handbook of Physical Properties for Hydrocarbons and Chemicals: Physical Properties for More Than 54,000 Organic and Inorganic Chemical Compounds, Coverage for C1 to C100 Organics and Ac to Zr Inorganics |date=6 January 2015 |publisher=[[Gulf Professional Publishing]] |isbn=978-0-12-801146-1 |page=718 |url=https://books.google.com/books?id=GutDBAAAQBAJ&dq=iodine+dioxide+IO2&pg=PA718 |access-date=10 May 2023 |language=en}}</ref><ref>{{cite book |last1=Haynes |first1=William M. |title=CRC Handbook of Chemistry and Physics |date=19 April 2016 |publisher=[[CRC Press]] |isbn=978-1-4398-8050-0 |page=2-17 |url=https://books.google.com/books?id=c1rNBQAAQBAJ&dq=iodine+dioxide+IO2&pg=SA2-PA17 |access-date=10 May 2023 |language=en}}</ref> Only stable as a dilute gas,<ref name=Particles/> this compound is one of many [[iodine oxide]]s,<ref>{{cite book |last1=De |first1=Anil Kumar |title=A Textbook Of Inorganic Chemistry |date=2007 |publisher=New Age International |isbn=978-81-224-1384-7 |page=584 |url=https://books.google.com/books?id=PpTi_JAx7PgC&dq=iodine+dioxide+IO2&pg=PA584 |access-date=10 May 2023 |language=en}}</ref><ref>{{cite book |last1=Parks |first1=Lytle Raymond |title=Systematic College Chemistry |date=1952 |publisher=Blakiston Company |page=304 |url=https://books.google.com/books?id=ftJTuxEUISgC&q=iodine+dioxide+IO2 |access-date=10 May 2023 |language=en}}</ref> and "iodine dioxide" is sometimes used to describe its formal [[dimer (chemistry)|dimer]], the salt [[diiodine tetroxide]] (I<sub>2</sub>O<sub>4</sub>, [IO]<sup> |
'''Iodine dioxide''' is a binary [[inorganic compound]] of [[iodine]] and [[oxygen]] with the chemical formula {{chem|I|O|2}}.<ref>{{cite book |last1=Yaws |first1=Carl |title=The Yaws Handbook of Physical Properties for Hydrocarbons and Chemicals: Physical Properties for More Than 54,000 Organic and Inorganic Chemical Compounds, Coverage for C1 to C100 Organics and Ac to Zr Inorganics |date=6 January 2015 |publisher=[[Gulf Professional Publishing]] |isbn=978-0-12-801146-1 |page=718 |url=https://books.google.com/books?id=GutDBAAAQBAJ&dq=iodine+dioxide+IO2&pg=PA718 |access-date=10 May 2023 |language=en}}</ref><ref>{{cite book |last1=Haynes |first1=William M. |title=CRC Handbook of Chemistry and Physics |date=19 April 2016 |publisher=[[CRC Press]] |isbn=978-1-4398-8050-0 |page=2-17 |url=https://books.google.com/books?id=c1rNBQAAQBAJ&dq=iodine+dioxide+IO2&pg=SA2-PA17 |access-date=10 May 2023 |language=en}}</ref> Only stable as a dilute gas,<ref name=Particles/> this compound is one of many [[iodine oxide]]s,<ref>{{cite book |last1=De |first1=Anil Kumar |title=A Textbook Of Inorganic Chemistry |date=2007 |publisher=New Age International |isbn=978-81-224-1384-7 |page=584 |url=https://books.google.com/books?id=PpTi_JAx7PgC&dq=iodine+dioxide+IO2&pg=PA584 |access-date=10 May 2023 |language=en}}</ref><ref>{{cite book |last1=Parks |first1=Lytle Raymond |title=Systematic College Chemistry |date=1952 |publisher=Blakiston Company |page=304 |url=https://books.google.com/books?id=ftJTuxEUISgC&q=iodine+dioxide+IO2 |access-date=10 May 2023 |language=en}}</ref> and "iodine dioxide" is sometimes used to describe its formal [[dimer (chemistry)|dimer]], the salt [[diiodine tetroxide]] (I<sub>2</sub>O<sub>4</sub>, [IO]<sup>+</sup>[IO<sub>3</sub>]<sup>−</sup>). |
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It is formed, in [[parts-per-trillion]] quantities,<ref>{{cite journal|last1=Saiz-Lopez|first1=A.|last2=Fernandez|first2=R. P.|last3=Ordóñez|first3=C.|last4=Kinnison|first4=D. E.|last5=Gómez Martín|first5=J. C.|last6=Lamarque|first6=J.-F.|last7=Tilmes|first7=S.|title=Iodine chemistry in the troposphere and its effect on ozone|journal=Atmospheric Chemistry and Physics|date=10 December 2014|volume=14|issue=23|pages=13119–13143|doi=10.5194/acp-14-13119-2014|bibcode=2014ACP....1413119S|doi-access=free|hdl=11336/100317|hdl-access=free}}</ref> at the [[marine boundary layer]] and believed to mediate [[particulate nucleation]] therein. The [[iodine]], originally from algaeic [[diiodomethane]], is [[photooxidation|photooxidized]] to [[iodine monoxide]], which then disproportionates to free iodine atoms and iodine dioxide. At a sufficiently large concentration, the particles then combine to form small grains of [[diiodine tetroxide]].<ref name=Particles>{{cite journal|last1=Hoffmann|first1=Thorsten|last2=O'Dowd|first2=Colin D.|last3=Seinfeld|first3=John H.|title=Iodine oxide homogeneous nucleation: An explanation for coastal new particle production|journal=Geophysical Research Letters|date=15 May 2001|volume=28|issue=10|pages=1949–1952|doi=10.1029/2000GL012399|bibcode=2001GeoRL..28.1949H|url=https://authors.library.caltech.edu/50961/1/grl14261.pdf|doi-access=free}}</ref><ref>{{cite journal|last1=Cox|first1=R. A.|last2=Bloss|first2=W. J.|last3=Jones|first3=R. L.|last4=Rowley|first4=D. M.|title=OIO and the atmospheric cycle of iodine|journal=Geophysical Research Letters|date=1 July 1999|volume=26|issue=13|pages=1857–1860|doi=10.1029/1999GL900439|bibcode=1999GeoRL..26.1857C|s2cid=128402214 |url=http://pure-oai.bham.ac.uk/ws/files/11849889/Cox_OIO_and_the_Atmospheric_Cycle_of_Iodine_GRL_1999.pdf}}</ref> |
It is formed, in [[parts-per-trillion]] quantities,<ref>{{cite journal|last1=Saiz-Lopez|first1=A.|last2=Fernandez|first2=R. P.|last3=Ordóñez|first3=C.|last4=Kinnison|first4=D. E.|last5=Gómez Martín|first5=J. C.|last6=Lamarque|first6=J.-F.|last7=Tilmes|first7=S.|title=Iodine chemistry in the troposphere and its effect on ozone|journal=Atmospheric Chemistry and Physics|date=10 December 2014|volume=14|issue=23|pages=13119–13143|doi=10.5194/acp-14-13119-2014|bibcode=2014ACP....1413119S|doi-access=free|hdl=11336/100317|hdl-access=free}}</ref> at the [[marine boundary layer]] and believed to mediate [[particulate nucleation]] therein. The [[iodine]], originally from algaeic [[diiodomethane]], is [[photooxidation|photooxidized]] to [[iodine monoxide]], which then disproportionates to free iodine atoms and iodine dioxide. At a sufficiently large concentration, the particles then combine to form small grains of [[diiodine tetroxide]].<ref name=Particles>{{cite journal|last1=Hoffmann|first1=Thorsten|last2=O'Dowd|first2=Colin D.|last3=Seinfeld|first3=John H.|title=Iodine oxide homogeneous nucleation: An explanation for coastal new particle production|journal=Geophysical Research Letters|date=15 May 2001|volume=28|issue=10|pages=1949–1952|doi=10.1029/2000GL012399|bibcode=2001GeoRL..28.1949H|url=https://authors.library.caltech.edu/50961/1/grl14261.pdf|doi-access=free}}</ref><ref>{{cite journal|last1=Cox|first1=R. A.|last2=Bloss|first2=W. J.|last3=Jones|first3=R. L.|last4=Rowley|first4=D. M.|title=OIO and the atmospheric cycle of iodine|journal=Geophysical Research Letters|date=1 July 1999|volume=26|issue=13|pages=1857–1860|doi=10.1029/1999GL900439|bibcode=1999GeoRL..26.1857C|s2cid=128402214 |url=http://pure-oai.bham.ac.uk/ws/files/11849889/Cox_OIO_and_the_Atmospheric_Cycle_of_Iodine_GRL_1999.pdf}}</ref> |
Latest revision as of 03:07, 26 November 2024
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Names | |
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Other names
dioxidoiodide, iodyl, iodoxy radical, iodine peroxide, iodine superoxide
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Identifiers | |
3D model (JSmol)
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ChEBI | |
ChemSpider | |
404604 | |
PubChem CID
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Properties | |
IO2 | |
Molar mass | 158.902 g·mol−1 |
Appearance | yellow solid |
Density | 4.2 g/cm3 |
Melting point | 130 °C (266 °F; 403 K) |
reacts with water | |
Except where otherwise noted, data are given for materials in their standard state (at 25 °C [77 °F], 100 kPa).
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Iodine dioxide is a binary inorganic compound of iodine and oxygen with the chemical formula IO
2.[1][2] Only stable as a dilute gas,[3] this compound is one of many iodine oxides,[4][5] and "iodine dioxide" is sometimes used to describe its formal dimer, the salt diiodine tetroxide (I2O4, [IO]+[IO3]−).
It is formed, in parts-per-trillion quantities,[6] at the marine boundary layer and believed to mediate particulate nucleation therein. The iodine, originally from algaeic diiodomethane, is photooxidized to iodine monoxide, which then disproportionates to free iodine atoms and iodine dioxide. At a sufficiently large concentration, the particles then combine to form small grains of diiodine tetroxide.[3][7]
References
[edit]- ^ Yaws, Carl (6 January 2015). The Yaws Handbook of Physical Properties for Hydrocarbons and Chemicals: Physical Properties for More Than 54,000 Organic and Inorganic Chemical Compounds, Coverage for C1 to C100 Organics and Ac to Zr Inorganics. Gulf Professional Publishing. p. 718. ISBN 978-0-12-801146-1. Retrieved 10 May 2023.
- ^ Haynes, William M. (19 April 2016). CRC Handbook of Chemistry and Physics. CRC Press. p. 2-17. ISBN 978-1-4398-8050-0. Retrieved 10 May 2023.
- ^ a b Hoffmann, Thorsten; O'Dowd, Colin D.; Seinfeld, John H. (15 May 2001). "Iodine oxide homogeneous nucleation: An explanation for coastal new particle production" (PDF). Geophysical Research Letters. 28 (10): 1949–1952. Bibcode:2001GeoRL..28.1949H. doi:10.1029/2000GL012399.
- ^ De, Anil Kumar (2007). A Textbook Of Inorganic Chemistry. New Age International. p. 584. ISBN 978-81-224-1384-7. Retrieved 10 May 2023.
- ^ Parks, Lytle Raymond (1952). Systematic College Chemistry. Blakiston Company. p. 304. Retrieved 10 May 2023.
- ^ Saiz-Lopez, A.; Fernandez, R. P.; Ordóñez, C.; Kinnison, D. E.; Gómez Martín, J. C.; Lamarque, J.-F.; Tilmes, S. (10 December 2014). "Iodine chemistry in the troposphere and its effect on ozone". Atmospheric Chemistry and Physics. 14 (23): 13119–13143. Bibcode:2014ACP....1413119S. doi:10.5194/acp-14-13119-2014. hdl:11336/100317.
- ^ Cox, R. A.; Bloss, W. J.; Jones, R. L.; Rowley, D. M. (1 July 1999). "OIO and the atmospheric cycle of iodine" (PDF). Geophysical Research Letters. 26 (13): 1857–1860. Bibcode:1999GeoRL..26.1857C. doi:10.1029/1999GL900439. S2CID 128402214.