Journal
ATMOSPHERIC ENVIRONMENT
Volume 127, Issue -, Pages 80-89Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2015.12.033
Keywords
Rate coefficient; Mechanism; Kinetics; Atmospheric implications; Ether
Funding
- Consejeria de Ciencia y Tecnologia de la Junta de Comunidades de Castilla-La Mancha [PII1I09-0202-3992]
- Ministerio de Ciencia e Innovacion [ENE2007-67529CO2-02]
- SECyT-UNC [05/C146]
- Santander Foundation
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Rate coefficients at room temperature and atmospheric pressure for the reaction of isopropenyl methyl ether (i-PME) (CH2=C(CH3)OCH3), with OH and NO3 radicals and with Cl atoms have been determined in a 50 L Pyrex glass reaction chamber in conjunction with Fourier Transform Infrared absorption spectroscopy (FTIR) as a detection technique. The chamber is equipped with a White-type multiple-reflection mirror system with a total optical path length of approximate to 200 m. Additional experiments were carried out using evacuable Teflon-coated bags (volume 150 L) and a gas chromatography/mass spectrometry-time of flight (GC-TOF MS) detection system. This is the first kinetic study carried out to date for these reactions. The rate coefficients k (in units of cm(3) molecule(-1) s(-1)) obtained are: (1.14 +/- 0.10) x 10(-10) for the OH reaction, (2.41 +/- 0.50) x 10(-11), for the NO3 reaction and (7.03 +/- 0.67) x 10(-10) for the Cl reaction. A mechanism is proposed from the observed reaction products. The atmospheric lifetimes of the studied ether is estimated considering the rate coefficients of the reactions with OH and NO3 radicals and Cl atom. Calculated atmospheric lifetimes reveal that the dominant loss process for i-PME is clearly the night-time reaction with the NO3 radical. The radiative efficiency (RE) is obtained from the infrared spectra of the ether and the global warming potential (GWP) is then estimated. Atmospheric implications of the ether emission are discussed. (C) 2015 Elsevier Ltd. All rights reserved.
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