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 AbstractRepresentation of binary pheromone blends by glomerulus-specific olfactory projection neurons    Next AbstractTransport of hop aroma compounds across Caco-2 monolayers »

Environ Sci Technol


Title:"The Ozonolysis of Methylated Selenide Compounds in the Atmosphere: Isotopes, Kinetics, Products, and Mechanisms"
Author(s):Heine PA; Borduas-Dedekind N;
Address:"Department of Chemistry, University of British-Columbia, Vancouver, BC V6T 1Z1, Canada"
Journal Title:Environ Sci Technol
Year:2023
Volume:20230821
Issue:35
Page Number:13079 - 13087
DOI: 10.1021/acs.est.3c01586
ISSN/ISBN:1520-5851 (Electronic) 0013-936X (Linking)
Abstract:"Selenium (Se) is an essential micronutrient with an important atmospheric component in its biogeochemical cycle. In this cycle, phytoplankton form volatile organic Se species, such as dimethyl selenide (CH(3)SeCH(3)) and dimethyl diselenide (CH(3)SeSeCH(3)), which are emitted into the atmosphere. To predict the atmospheric fate of these methylated Se compounds, we investigated their ozonolysis reaction. We used proton-transfer-reaction time-of-flight mass spectrometry to quantify atmospheric Se and its isotopes, and used this method in kinetic and product studies. The ozonolysis of CH(3)SeCH(3) proceeded with a rate constant of (7.4 +/- 2.2) x 10(-17) cm(3) molec(-1) s(-1) at 26 +/- 1 degrees C with an activation energy of 50 +/- 14 kJ mol(-1) forming dimethyl selenoxide (CH(3)Se(O)CH(3)). Comparatively, CH(3)SeSeCH(3) reacted with O(3) at (2.6 +/- 0.9) x 10(-17) cm(3) molec(-1) s(-1) at 27 +/- 1 degrees C with an activation energy of 56 +/- 5 kJ mol(-1) forming methylselinic acid (CH(3)Se(O)OH). At 20 ppbv of O(3), the atmospheric lifetimes of CH(3)SeCH(3) and CH(3)SeSeCH(3) are 7.6 and 22 h, respectively. The Se oxidation products were confirmed by synthesis and can serve as new atmospheric tracers of methylated Se compounds. Overall, we measured Se isotopes in real time and determined the rate constants, activation energies, and oxidation products. These mechanisms can now be used to determine the quantitative atmospheric fate of Se toward O(3), and thus its distribution within a changing climate"
Keywords:Kinetics Atmosphere *Selenium Isotopes *Ozone atmospheric lifetime dimethyl diselenide dimethyl selenide oxidation ozone rate constant selenium;
Notes:"MedlineHeine, Paul A Borduas-Dedekind, Nadine eng Research Support, Non-U.S. Gov't 2023/08/21 Environ Sci Technol. 2023 Sep 5; 57(35):13079-13087. doi: 10.1021/acs.est.3c01586. Epub 2023 Aug 21"

 
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 05-11-2024