Daytime reactions of 1,8-cineole in the troposphere

Chemphyschem. 2011 Aug 1;12(11):2145-54. doi: 10.1002/cphc.201100077. Epub 2011 Jun 14.

Abstract

Relative rate coefficients for the gas-phase reaction of chlorine atoms (Cl) and hydroxyl radicals (OH) with 1,8-cineole were determined by Fourier-transform infrared (FTIR) spectroscopy between 285 and 313 K at atmospheric pressure. The temperature dependence of both reactions shows simple Arrhenius behaviour which can be represented by the following expressions (in units of cm(3) molecule(-1) s(-1)): k(1,8-cineole+OH)=(6.28 ± 6.53) × 10(-8) exp[(-2549.3 ± 155.7)/T] and k(1,8-cineole+Cl)=(1.35 ± 1.07) × 10(-10) exp[(-151.6 ± 237.7)/T]. Major products of the titled reactions were identified by solid-phase microextraction (SPME) coupled to a GC-MS. Additionally, the first step of the reaction was theoretically studied by ab initio calculations and a reaction mechanism is proposed.

Publication types

  • Research Support, Non-U.S. Gov't

MeSH terms

  • Atmospheric Pressure
  • Chlorine / chemistry
  • Cyclohexanols / chemistry*
  • Eucalyptol
  • Gases / chemistry
  • Hydroxyl Radical / chemistry
  • Kinetics
  • Models, Molecular
  • Monoterpenes / chemistry*
  • Spectroscopy, Fourier Transform Infrared
  • Temperature
  • Thermodynamics

Substances

  • Cyclohexanols
  • Gases
  • Monoterpenes
  • Hydroxyl Radical
  • Chlorine
  • Eucalyptol