A Possible Mechanism for Furan Formation in the Tropospheric Oxidation of Dienes

The isoprene + OH gas-phase reaction has been widely studied because of its relevance in tropospheric chemistry. However, an unsolved question remains concerning the mechanism for the formation of the observed 3-methylfuran. OH addition to dienes, such as isoprene and butadiene, is assumed to occur...

Full description

Saved in:
Bibliographic Details
Published inEnvironmental science & technology Vol. 39; no. 22; pp. 8797 - 8802
Main Authors Francisco-Márquez, Misaela, Alvarez-Idaboy, J. Raúl, Galano, Annia, Vivier-Bunge, Annik
Format Journal Article
LanguageEnglish
Published Washington, DC American Chemical Society 15.11.2005
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:The isoprene + OH gas-phase reaction has been widely studied because of its relevance in tropospheric chemistry. However, an unsolved question remains concerning the mechanism for the formation of the observed 3-methylfuran. OH addition to dienes, such as isoprene and butadiene, is assumed to occur only at the external carbon atoms, thus restricting furan formation to a step after addition at C1 and C4. Moreover, cyclization of the carbon chain necessarily involves a cis conformation. In this work, several quantum chemistry methods have been used to model five different reaction paths for furan formation. A mechanism that is highly favored for intermediates that do not undergo collisional stabilization has been identified.
Bibliography:ark:/67375/TPS-RJ1DL5XV-F
istex:B36A03FA20E2B297F8E9D30BF20D49C922212990
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0013-936X
1520-5851
DOI:10.1021/es0500714