The products formed by the hydroxyl radical initiated photo-oxidation of diethyl ether have been investigated by irradiating synthetic air mixtures containing diethyl ether and nitrous acid in amounts approaching ppbv levels in a smog chamber. The decay of reactants and formation of products were monitored by gas chromatography, HPLC, and by chemiluminescent analysis. The major products are ethyl formate and formaldehyde, minor products include ethyl acetate, acetaldehyde, peroxyacetyl nitrate, methyl nitrate, and ethyl nitrate. The products observed arise from the decomposition reactions of the l-ethoxyethoxy radical and its reaction with oxygen. One molecule of nitric oxide appears to be oxidized per molecule of diethyl ether reacted. This is lower than would be expected on the basis of the proposed mechanism and possible reasons for the discrepancy are discussed. 0 1993 John Wiley & Sons, Inc.
The rate coefficients for the gas-phase reactions of allyl-,
tert-butyl-, cyclopentyl-, and 2-pentylperoxy
radicals
with NO have been measured at 297 ± 2 K in a flow tube reactor using
chemical ionization mass spectrometric
(CIMS) detection of the peroxy radical. The hydrocarbon radicals
were produced through the dissociation of
the parent alkyl iodide in a low-power radio frequency (rf) discharge.
The unimolecular decomposition of
the c-pentyl radicals in the rf discharge yielded allyl
radicals. The peroxy radicals were generated by
reacting
the hydrocarbon radicals with O2. The rate
coefficients were found to be, in units of
10-12 cm3
molecule-1
s-1, 10.5 ± 1.8, 7.9 ± 1.3, 10.9 ± 1.9,
and 8.0 ± 1.4 for the reactions of NO with
CH2CHCH2O2,
t-C4H9O2,
c-C5H9O2, and
2-C5H11O2 radicals, respectively.
The results of this study together with our previous
results
for nonsubstituted C1−C3 alkyl peroxy
radicals suggest no significant trend in the rate coefficients with
size
and branching of the radicals. This is in contradiction to some
previous studies, which found that the rate
coefficients decrease with increasing radical size and complexity.
Some implications of this finding for
atmospheric chemistry are briefly discussed.
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