NOx-Air Photooxidations of C5-C8 n-Alkanes
J. Phys. Chem. A, Vol. 105, No. 6, 2001 1027
The above CH3ONO/NO/n-alkane/air irradiations with a
single n-alkane present also showed the formation (numbers in
parentheses are the percents relative to the Cn-hydroxyalkyl
nitrate) of C5- (3%), C6- (3%), and C7-hydroxyalkyl nitrates
(7%) from the n-octane reaction, C5- (1.5%) and C6-hydroxy-
alkyl nitrates (6.5%) from the n-heptane reaction, and C5-
hydroxyalkyl nitrates (9%) from the n-hexane reaction. In two
of the experiments with all four n-alkanes present, CH3CH-
(OH)CH(ONO2)CH3 was formed in situ from the reaction of
the OH radical with cis-2-butene and used as an internal standard
for hydroxyalkyl nitrate quantification, and in the three ad-
ditional experiments the relative yields of hydroxyalkyl nitrates
from the four n-alkanes were measured. The hydroxyalkyl nitrate
formation yields resulting from these experiments are also given
in Table 4. It is of interest to note that the API-MS is quite
sensitive to hydroxyalkyl nitrates (more so than to hydroxy-
carbonyls, as evident from Figure 6 and the formation yield
data shown in Table 4), with (Figure 6) detection limits of <50
part-per-trillion (ppt) mixing ratio (<1 × 109 molecule cm-3);
indeed, dilution of the chamber contents by a factor of 8
indicated that 10 ppt mixing ratios (2 × 108 molecule cm-3) of
these hydroxyalkyl nitrates could still be readily observed.
Contract No. 97-312. The statements and conclusions are those
of the authors and not necessarily those of the California Air
Resources Board.
References and Notes
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Our alkyl nitrate, hydroxyalkyl nitrate, and hydroxycarbonyl
formation yields given in Table 4, combined with the literature
carbonyl yields arising from alkoxy radical decomposition and
reaction with O2, account for ∼95%, ∼80%, ∼70%, and ∼55%
of the products formed from the OH radical-initiated reactions
of n-pentane, n-hexane, n-heptane, and n-octane (in the presence
of NO), respectively, with uncertainties of approximately a factor
of 1.4 in each case. We can therefore now account for most of
the reaction products formed from these n-alkanes, and hy-
droxycarbonyl formation accounts for a significant fraction of
these products (in fact, for most of the products from n-hexane,
n-heptane, and n-octane). Hydroxyalkyl nitrate formation ac-
counts for a few percent of the overall reaction products, and is
consistently ∼25% of the corresponding alkyl nitrate yields.
Our hydroxyalkyl nitrate yield from the n-hexane reaction of
0.046 (with an uncertainty of a factor of 2) is reasonably
consistent with the approximate upper limit estimate of Eberhard
et al.15 for the formation of 5-nitrooxyhexan-2-ol of 0.03-0.04.
Thus significant fractions of the atmospheric reaction products
of gC5 n-alkanes (and other alkanes whose intermediate alkoxy
radicals can isomerize) are comprised of hydroxycarbonyls and
hydroxyalkyl nitrates, compound classes which are presently
difficult to analyze under atmospheric conditions.
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J. EnViron. Sci. Technol. 1999, 33, 3586.
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Acknowledgment. The authors gratefully thank the Cali-
fornia Air Resources Board for supporting this research through