Unsaturated ethers are widely used in different industries. Allyl ethers (ROCH2CH=CH2) and vinyl ethers (ROCH=CH2), where R is an alkyl group, are mainly used as raw material for epoxy silane coupling agents and unsaturated polyesters containing allyl groups, in cosmetics, for manufacturing of coatings and in the preparation of fragances1. Even though an evaluation of the amount of the world production of these compounds is not available at present, their uses certainly results in their release into the atmosphere.
While the OH radical is considered to be the major daytime oxidant, chlorine atoms present at an average global concentration of ~1x104 atoms cm-3 2, can play an important role in atmospheric chemistry since atomic Cl usually reacts with volatile organic compounds (VOCs) with a much greater rate constant than OH radicals3. Moreover, in the coastal urban areas the concentrations of Cl atoms, for a brief period at dawn in the marine boundary layer, are estimated to be significantly large, as high as 105 atoms cm-3 or more4,5. Thus, reactions with Cl atoms in coastal areas may represent a significant loss process for VOCs.
The aim of this study was to extend the existing scant data base of rate constants for the reactions of chlorine atoms with allyl and vinyl ethers, as part of ongoing work in our laboratory regarding the atmospheric impact of these oxygenated compounds. The relative rate method was used to study the following reactions:
Cl + CH2=CHCH2OCH2CH3 ---> Products (1)
Cl + CH2=CHCH2OCH2CH=CH2 ---> Products (2)
Cl + CH2=CHOCH2CH2Cl ---> Products (3)
Relative rate constants were measured by comparing the Cl atom reaction rate with the ethers to that with n-pentane used as the reference compound. All the experiments were carried out in an
Based on the rate constants reported above, the tropospheric lifetimes of the three ethers were calculated as: 2 days for CH2=CHCH2OCH2CH3 , 3.3 days for CH2=CHCH2OCH2CH=CH2 , and > 115 days for CH2=CHOCH2CH2Cl, taking an average global concentration of 1x104 atoms cm-3 for Cl atoms. These relatively short lifetimes indicate that these compounds will be oxidised rapidly near their anthropogenic sources, thus making a negligible contribution to global warming but probably increasing local atmospheric pollution.
1. Perstorp web site: www.perstorp.com and BASF web site. www.basf.de.
2. O.W. Wingenter, M.K. Kubo, N.J. Blake, T.W. Smith, D.R. Blake, F.S. Rowland , J. Geophys. Res. 101 (1996) 4331-4340.
3. B.J. Finlayson-Pitts, C.J. Keoshian, B. Buehler, A.A. Ezell, Int. J. Chem. Kinet. 31 (1999) 491-499.
6. NIST-Chemical Kinetics Database on the Web, 2002. Standard Reference Database 17, Version 7.0 (Web Version), Release 1.2.