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 AbstractRedundant actions of neuropeptides encoded by the dh-pban gene for larval color pattern formation in the oriental armyworm Mythimnaseparata    Next AbstractRapid evolution of sex pheromone-producing enzyme expression in Drosophila »

Proc Natl Acad Sci U S A


Title:Size distribution dynamics reveal particle-phase chemistry in organic aerosol formation
Author(s):Shiraiwa M; Yee LD; Schilling KA; Loza CL; Craven JS; Zuend A; Ziemann PJ; Seinfeld JH;
Address:"Divisions of Chemistry and Chemical Engineering and Engineering, California Institute of Technology, Pasadena, CA 91125, USA"
Journal Title:Proc Natl Acad Sci U S A
Year:2013
Volume:20130701
Issue:29
Page Number:11746 - 11750
DOI: 10.1073/pnas.1307501110
ISSN/ISBN:1091-6490 (Electronic) 0027-8424 (Print) 0027-8424 (Linking)
Abstract:"Organic aerosols are ubiquitous in the atmosphere and play a central role in climate, air quality, and public health. The aerosol size distribution is key in determining its optical properties and cloud condensation nucleus activity. The dominant portion of organic aerosol is formed through gas-phase oxidation of volatile organic compounds, so-called secondary organic aerosols (SOAs). Typical experimental measurements of SOA formation include total SOA mass and atomic oxygen-to-carbon ratio. These measurements, alone, are generally insufficient to reveal the extent to which condensed-phase reactions occur in conjunction with the multigeneration gas-phase photooxidation. Combining laboratory chamber experiments and kinetic gas-particle modeling for the dodecane SOA system, here we show that the presence of particle-phase chemistry is reflected in the evolution of the SOA size distribution as well as its mass concentration. Particle-phase reactions are predicted to occur mainly at the particle surface, and the reaction products contribute more than half of the SOA mass. Chamber photooxidation with a midexperiment aldehyde injection confirms that heterogeneous reaction of aldehydes with organic hydroperoxides forming peroxyhemiacetals can lead to a large increase in SOA mass. Although experiments need to be conducted with other SOA precursor hydrocarbons, current results demonstrate coupling between particle-phase chemistry and size distribution dynamics in the formation of SOAs, thereby opening up an avenue for analysis of the SOA formation process"
Keywords:"Aerosols/*chemistry Aldehydes/chemistry Alkanes/chemistry Atmosphere/*analysis Carbon/analysis Kinetics *Models, Chemical Oxidation-Reduction Oxygen/analysis Particle Size Photochemistry Volatile Organic Compounds/*chemistry alkane gas-particle interactio;"
Notes:"MedlineShiraiwa, Manabu Yee, Lindsay D Schilling, Katherine A Loza, Christine L Craven, Jill S Zuend, Andreas Ziemann, Paul J Seinfeld, John H eng Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S. 2013/07/03 Proc Natl Acad Sci U S A. 2013 Jul 16; 110(29):11746-50. doi: 10.1073/pnas.1307501110. Epub 2013 Jul 1"

 
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 26-12-2024