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 AbstractBlue light exposure and nutrient conditions influence the expression of genes involved in simultaneous hyphal knot formation in Coprinopsis cinerea    Next AbstractAnt Lasius niger joining one-way trails go against the flow »

J Phys Chem Lett


Title:Kinetics Study of OH Uptake onto Deliquesced NaCl Particles by Combining Laser Photolysis and Laser-Induced Fluorescence
Author(s):Sakamoto Y; Zhou J; Kohno N; Nakagawa M; Hirokawa J; Kajii Y;
Address:"Center for Regional Environmental Research , National Institute for Environmental Studies , Ibaraki 305-8506 , Japan. Faculty of Environmental Earth Science , Hokkaido University , Sapporo 060-0810 , Japan"
Journal Title:J Phys Chem Lett
Year:2018
Volume:20180711
Issue:14
Page Number:4115 - 4119
DOI: 10.1021/acs.jpclett.8b01725
ISSN/ISBN:1948-7185 (Electronic) 1948-7185 (Linking)
Abstract:"Despite the role of hydroxyl radical (OH) uptake onto sea-salt particles as a daytime chlorine source, affecting the chemical processes in the marine boundary layer, its uptake coefficient has not yet been confirmed by direct measurement methods. This study reports the application of a combination technique of laser flash photolysis generation and laser-induced fluorescence detection for the direct kinetic measurement of OH uptake onto deliquesced NaCl particles. The uptake coefficient was not constant and inversely depended on the initial OH concentration, indicating that the first uptake step is Langmuir-type adsorption. The resistance model, including surface processes, well reproduced the observed uptake coefficient. The model predicted an uptake coefficient for the atmospheric relevant OH concentration within the range from 0.77 to 0.95. Such values may lead to emissions of Cl(2) higher than those predicted in previous studies based on other values. Hence, the proposed value may provide more reliable estimations of ozone formation, oxidation of volatile organic compounds, secondary organic aerosol formation, and lifetime of methane and elemental mercury in the marine boundary layer"
Keywords:
Notes:"PubMed-not-MEDLINESakamoto, Yosuke Zhou, Jun Kohno, Nanase Nakagawa, Maho Hirokawa, Jun Kajii, Yoshizumi eng 2018/07/07 J Phys Chem Lett. 2018 Jul 19; 9(14):4115-4119. doi: 10.1021/acs.jpclett.8b01725. Epub 2018 Jul 11"

 
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 29-12-2024