Title of article :
The rate and mechanism of the gas-phase oxidation of hydroxyacetone
Author/Authors :
John J. Orlando، نويسنده , , Geoffrey S. Tyndall، نويسنده , , Jean-Marc Fracheboud، نويسنده , , Edgar G. Estupi?an، نويسنده , , Sylviane Haberkorn، نويسنده , , Audrey Zimmer، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 1998
Abstract :
The rate and mechanism for gas-phase destruction of hydroxyacetone, CH3C(O)CH2OH, by reaction with OH, Cl-atoms, and by photolysis have been determined. The first quantitative UV absorption spectrum of hydroxyacetone is reported over the wavelength range 235 to 340 nm; the spectrum is blue-shifted by about 15 nm relative to that of acetone and peaks at 266 nm, with a maximum absorption cross section of (6.7±0.6) ×10-20 cm2 molecule-1. Measurable absorption extends out to about 330 nm. The quantum yield for photolysis of hydroxyacetone in the region relevant to the troposphere (λ>290 nm) was found to be significantly less than unity. Rate coefficients for the reaction of hydroxyacetone with OH radicals and Cl-atoms were determined at 298 K using the relative rate technique. The rate coefficient for reaction with OH was found to be (3.0±0.7)×10-12 cm3 molecule-1 s-1, while the rate coefficient for reaction with Cl-atoms was found to be (5.6±0.7)×10-11 cm3 molecule-1 s-1. Both values agree well with previous studies. The data were used to determine the lifetime of hydroxyacetone in the troposphere. Reaction with OH is the major gas-phase destruction mechanism for this compound, limiting its lifetime to about 4 days, while photolysis is found to be only of minor importance
Keywords :
Hydroxyacetone: Biogenic hydrocarbons: Oxidation: Photochemistry
Journal title :
Atmospheric Environment
Journal title :
Atmospheric Environment