“Criegee intermediate”的意思、由来-开放百科全书

A Criegee intermediate (also called a Criegee zwitterion or Criegee biradical) is a molecule containing the oxide of a carbonyl group. These chemicals may react with sulfur dioxide and nitrogen oxides in the earth's atmosphere, and are implicated in the formation of aerosols, which are an important factor in controlling global climate.^[1]^[2] Criegee intermediates are also an important source of OH (hydroxyl radicals).^[3] OH radicals are the most important oxidant in the troposphere,^[4] and are important in controlling air quality and pollution.

The formation of this sort of structure was first postulated in the 1950s by Rudolf Criegee,^[5] for whom it is named, but it was not until 2012 that direct detection of such chemicals was reported.^[6] Infrared spectroscopy suggests the electronic structure has a substantially zwitterionic character rather than the biradical character that had previously been proposed.^[7]

Formation

Criegee intermediates are formed by the gas-phase reactions of alkenes and ozone in the earth's atmosphere. Ozone adds across the carbon–carbon double bond of the alkene to form a primary ozonide, which then decomposes to produce a carbonyl (RR'CO) and a carbonyl oxide. The latter is known as the Criegee intermediate.^[8]

The alkene ozonolysis reaction is extremely exothermic, releasing about {{convert|50|kcal/mol|kJ/mol}} of excess energy. Therefore, the Criegee intermediates are formed with a large amount of internal energy.^[8]

Removal

When Criegee intermediates are formed, some portion of them will undergo prompt unimolecular decay, producing OH radicals and other products. However, they may instead become stabilized by interactions with other molecules or reacted with other chemicals to give different products.

Criegee intermediates may be collisionally stabilized via collisions with other molecules in the atmosphere. These stabilized Criegee intermediates may then undergo thermal unimolecular decay to OH radicals and other products, or may undergo bimolecular reactions with other atmospheric species.

In the ozonolysis reaction sequence, the Criegee intermediate reacts with another carbonyl compound (generally the aldehyde or ketone byproduct of the Criegee-intermediate formation reaction itself) to form a molozonide.

References

1. ^{{cite journal |first1= Oliver |last1= Welz |first2= John D. |last2= Savee |first3= David L. |last3= Osborn |first4= Subith S. |last4= Vasu |first5= Carl J. |last5= Percival |first6= Dudley E. |last6= Shallcross |first7= Craig A. |last7= Taatjes |title= Direct Kinetic Measurements of Criegee Intermediate (CH₂OO) Formed by Reaction of C₂I with O₂ |journal= Science |date= 13 January 2012 |volume= 335 |issue= 6065 |pages= 204–207 |doi= 10.1126/science.1213229 |pmid= 22246773 |bibcode = 2012Sci...335..204W }}
2. ^{{cite news| last=Castro| first=Joseph| title=How mysterious molecules may help cool Earth|url=http://www.msnbc.msn.com/id/45975663/ns/technology_and_science-science/#.TxCB1PmGmSo|publisher=MSNBC|accessdate=2012-01-12 |date= January 12, 2012 }}
3. ^{{Cite journal|last=Heard|first=Dwayne E.|last2=Whalley|first2=Lisa K.|last3=Stone|first3=Daniel|date=2012|title=Tropospheric OH and HO₂ radicals: field measurements and model comparisons|journal=Chemical Society Reviews|language=en|volume=41|issue=19|pages=6348–6404|doi=10.1039/C2CS35140D}}
4. ^{{Cite book|title=Chemistry of the upper and lower atmosphere : theory, experiments, and applications|last1=Finlayson-Pitts|first1=Barbara J.|last2=Pitts|first2=James N.|date=2000|publisher=Academic Press|isbn=9780080529073|location=San Diego|oclc=162128929}}
5. ^{{cite news| url=https://www.sciencedaily.com/releases/2012/01/120112142232.htm | title= Offsetting Global Warming: Molecule in Earth's Atmosphere Could 'Cool the Planet' | date= January 12, 2012| publisher= Science Daily | accessdate= 2012-01-14}}
6. ^{{Cite journal|last=Taatjes|first=Craig A.|last2=Shallcross|first2=Dudley E.|last3=Percival|first3=Carl J.|last4=Vasu|first4=Subith S.|last5=Osborn|first5=David L.|last6=Savee|first6=John D.|last7=Welz|first7=Oliver|date=2012-01-13|title=Direct Kinetic Measurements of Criegee Intermediate (CH₂OO) Formed by Reaction of CH₂I with O₂|journal=Science|language=en|volume=335|issue=6065|pages=204–207|doi=10.1126/science.1213229|issn=1095-9203|pmid=22246773}}
7. ^{{cite journal |title= Infrared Absorption Spectrum of the Simplest Criegee Intermediate CH₂OO |journal= Science |date= 12 April 2013 |volume= 340 |issue= 6129 |pages= 174–176 |doi= 10.1126/science.1234369 |pmid= 23580523 |last1= Su |first1= Yu-Te |last2= Huang |first2= Yu-Hsuan|authorlink3=Henryk Witek |last3= Witek |first3= Henryk A.|authorlink4=Yuan-Pern Lee |last4= Lee |first4= Yuan-Pern |bibcode = 2013Sci...340..174S }}
8. ^¹{{Cite journal|last=Marston|first=George|last2=Johnson|first2=David|date=2008-03-25|title=The gas-phase ozonolysis of unsaturated volatile organic compounds in the troposphere|journal=Chemical Society Reviews|language=en|volume=37|issue=4|pages=699–716|doi=10.1039/B704260B|pmid=18362978|issn=1460-4744}}