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« Previous AbstractIntegrating phase and composition of secondary organic aerosol from the ozonolysis of alpha-pinene    Next AbstractIdentification and characterization of a mammalian enzyme catalyzing the asymmetric oxidative cleavage of provitamin A »

Phys Chem Chem Phys


Title:New insights into secondary organic aerosol from the ozonolysis of alpha-pinene from combined infrared spectroscopy and mass spectrometry measurements
Author(s):Kidd C; Perraud V; Finlayson-Pitts BJ;
Address:"Department of Chemistry, University of California, Irvine, CA 92697, USA. bjfinlay@uci.edu"
Journal Title:Phys Chem Chem Phys
Year:2014
Volume:16
Issue:41
Page Number:22706 - 22716
DOI: 10.1039/c4cp03405h
ISSN/ISBN:1463-9084 (Electronic) 1463-9076 (Linking)
Abstract:"Understanding mechanisms of formation, growth and physical properties of secondary organic aerosol (SOA) is central to predicting impacts on visibility, health and climate. It has been known for many decades that the oxidation of monoterpenes by ozone in the gas phase readily forms particles. However, the species responsible for the initial nucleation and the subsequent growth are not well established. Recent studies point to high molecular weight highly oxygenated products with extremely low vapor pressures (ELVOC, extremely low volatility organic compounds) as being responsible for the initial nucleation, with more volatile species contributing to particle growth. We report here the results of studies of SOA formed in the ozonolysis of alpha-pinene in air at 297 +/- 2 K using atmospheric solids analysis probe (ASAP) mass spectrometry, attenuated total reflectance (ATR) Fourier transform infrared spectrometry and proton transfer reaction (PTR) mass spectrometry. Smaller particles are shown to be less volatile and have on average higher molecular mass components compared to larger particles, consistent with recent proposals regarding species responsible for the formation and growth of particles in this system. Thus the signatures of species responsible for particle development at various stages are observable even in particles of several hundred nm diameter. Pinonaldehyde and acetic acid were observed to evaporate from a film of impacted SOA at room temperature, from which the ratio of their diffusion coefficients to the square of the average film thickness, D/l(2), could be obtained. For acetic acid and pinonaldehyde, D/l(2) = 6.8 x 10(-6) s(-1) and 5.0 x 10(-6) s(-1) respectively, the relative magnitudes being consistent with the size difference between acetic acid and pinonaldehyde molecules. Limitations to quantifying the film thickness and hence absolute values of the diffusion coefficient are discussed and highlight a need for novel experimental methods for quantifying diffusion coefficients of organic species in SOA"
Keywords:
Notes:"PubMed-not-MEDLINEKidd, Carla Perraud, Veronique Finlayson-Pitts, Barbara J eng England 2014/09/19 Phys Chem Chem Phys. 2014 Nov 7; 16(41):22706-16. doi: 10.1039/c4cp03405h"

 
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