Bedoukian   RussellIPM   RussellIPM   Piezoelectric Micro-Sprayer


Home
Animal Taxa
Plant Taxa
Semiochemicals
Floral Compounds
Semiochemical Detail
Semiochemicals & Taxa
Synthesis
Control
Invasive spp.
References

Abstract

Guide

Alphascents
Pherobio
InsectScience
E-Econex
Counterpart-Semiochemicals
Print
Email to a Friend
Kindly Donate for The Pherobase

« Previous AbstractTesting the role of allelochemicals in different wheat cultivars to sustainably manage weeds    Next AbstractPupal mortality and adult emergence of western cherry fruit fly (Diptera: Tephritidae) exposed to the fungus Muscodor albus (Xylariales: Xylariaceae) »

J Phys Chem A


Title:Secondary organic aerosol formation from low-NO(x) photooxidation of dodecane: evolution of multigeneration gas-phase chemistry and aerosol composition
Author(s):Yee LD; Craven JS; Loza CL; Schilling KA; Ng NL; Canagaratna MR; Ziemann PJ; Flagan RC; Seinfeld JH;
Address:"Division of Engineering and Applied Science, California Institute of Technology, Pasadena, California 91125, United States"
Journal Title:J Phys Chem A
Year:2012
Volume:20120410
Issue:24
Page Number:6211 - 6230
DOI: 10.1021/jp211531h
ISSN/ISBN:1520-5215 (Electronic) 1089-5639 (Linking)
Abstract:"The extended photooxidation of and secondary organic aerosol (SOA) formation from dodecane (C(12)H(26)) under low-NO(x) conditions, such that RO(2) + HO(2) chemistry dominates the fate of the peroxy radicals, is studied in the Caltech Environmental Chamber based on simultaneous gas and particle-phase measurements. A mechanism simulation indicates that greater than 67% of the initial carbon ends up as fourth and higher generation products after 10 h of reaction, and simulated trends for seven species are supported by gas-phase measurements. A characteristic set of hydroperoxide gas-phase products are formed under these low-NO(x) conditions. Production of semivolatile hydroperoxide species within three generations of chemistry is consistent with observed initial aerosol growth. Continued gas-phase oxidation of these semivolatile species produces multifunctional low volatility compounds. This study elucidates the complex evolution of the gas-phase photooxidation chemistry and subsequent SOA formation through a novel approach comparing molecular level information from a chemical ionization mass spectrometer (CIMS) and high m/z ion fragments from an Aerodyne high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS). Combination of these techniques reveals that particle-phase chemistry leading to peroxyhemiacetal formation is the likely mechanism by which these species are incorporated in the particle phase. The current findings are relevant toward understanding atmospheric SOA formation and aging from the 'unresolved complex mixture,' comprising, in part, long-chain alkanes"
Keywords:
Notes:"PubMed-not-MEDLINEYee, Lindsay D Craven, Jill S Loza, Christine L Schilling, Katherine A Ng, Nga Lee Canagaratna, Manjula R Ziemann, Paul J Flagan, Richard C Seinfeld, John H eng 2012/03/20 J Phys Chem A. 2012 Jun 21; 116(24):6211-30. doi: 10.1021/jp211531h. Epub 2012 Apr 10"

 
Back to top
 
Citation: El-Sayed AM 2024. The Pherobase: Database of Pheromones and Semiochemicals. <http://www.pherobase.com>.
© 2003-2024 The Pherobase - Extensive Database of Pheromones and Semiochemicals. Ashraf M. El-Sayed.
Page created on 27-11-2024