PHYS 18 |
| Atomic chlorine is an important initiator of the atmospheric degradation of many oxygenated organic compounds, including ketones, particularly in marine environments. We have coupled laser flash photolysis of Cl2CO/ketone/N2 mixtures with time-resolved detection of Cl by atomic resonance fluorescence spectroscopy to investigate the kinetics of Cl reactions with acetone (R1), 2-butanone (R2), 3-pentanone (R3), and methylvinyl ketone (R4). R1, R2, and R3 proceed via H-transfer pathways. Observed temperature dependences of k1 – k3 are significantly different from those reported in the literature. R4 proceeds primarily by Cl addition to the double bond and, therefore, displays both temperature and pressure-dependent kinetics. Reversible adduct formation is observed at T ~ 425 K which, in conjunction with electronic structure calculations, allows the C–Cl bond strength in the product haloalkyl radical to be evaluated. Higher temperature studies aimed at characterizing the kinetics of H-transfer pathways for R4 are in progress and will be reported. |
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Physical Chemistry of Atmospheric Processes
8:00 AM-12:00 PM, Sunday, April 6, 2008 Morial Convention Center -- Rm. 343, Oral
Division of Physical Chemistry |