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 AbstractKey volatile compounds of 'Fuji Kiku' apples as affected by the storage conditions and shelf life: Correlation between volatile emission by intact fruit and juice extracted from the fruit    Next AbstractAssessing soil-air partitioning of PAHs and PCBs with a new fugacity passive sampler »

Faraday Discuss


Title:Critical factors determining the variation in SOA yields from terpene ozonolysis: a combined experimental and computational study
Author(s):Donahue NM; Hartz KE; Chuong B; Presto AA; Stanier CO; Rosenhorn T; Robinson AL; Pandis SN;
Address:"Department of Chemistry and Chemical Engineering, Carnegie Mellon University, Pittsburgh PA 15213, USA. nmd@andrew.cmu.edu"
Journal Title:Faraday Discuss
Year:2005
Volume:130
Issue:
Page Number:295 - 309
DOI: 10.1039/b417369d
ISSN/ISBN:1359-6640 (Print) 1359-6640 (Linking)
Abstract:"A substantial fraction of the total ultrafine particulate mass is comprised of organic compounds. Of this fraction, a significant subfraction is secondary organic aerosol (SOA), meaning that the compounds are a by-product of chemistry in the atmosphere. However, our understanding of the kinetics and mechanisms leading to and following SOA formation is in its infancy. We lack a clear description of critical phenomena; we often don't know the key, rate limiting steps in SOA formation mechanisms. We know almost nothing about aerosol yields past the first generation of oxidation products. Most importantly, we know very little about the derivatives in these mechanisms; we do not understand how changing conditions, be they precursor levels, oxidant concentrations, co-reagent concentrations (i.e., the VOC/NOx ratio) or temperature will influence the yields of SOA. In this paper we explore the connections between fundamental details of physical chemistry and the multitude of steps associated with SOA formation, including the initial gas-phase reaction mechanisms leading to condensible products, the phase partitioning itself, and the continued oxidation of the condensed-phase organic products. We show that SOA yields in the alpha-pinene + ozone are highly sensitive to NOx, and that SOA yields from beta-caryophylene + ozone appear to increase with continued ozone exposure, even as aerosol hygroscopicity increases as well. We suggest that SOA yields are likely to increase substantially through several generations of oxidative processing of the semi-volatile products"
Keywords:Aerosols/*chemistry Air Pollutants/*chemistry Mathematics Nitrogen Oxides/chemistry Organic Chemicals/*chemistry Oxidation-Reduction Ozone/*chemistry Temperature Terpenes/*chemistry;
Notes:"MedlineDonahue, Neil M Hartz, Kara E Huff Chuong, Bao Presto, Albert A Stanier, Charles O Rosenhorn, Thomas Robinson, Allen L Pandis, Spyros N eng Research Support, U.S. Gov't, Non-P.H.S. England 2005/09/16 Faraday Discuss. 2005; 130:295-309; discussion 363-86, 519-24. doi: 10.1039/b417369d"

 
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 22-11-2024