5078 J. Phys. Chem. A, Vol. 104, No. 21, 2000
Orlando et al.
energies below the estimated26 values, have recently reported
for the decomposition reactions of tert-butoxy28 and ethoxy29
radicals.
TABLE 1: Product Yields (Molar %) Measured in the
Cl-Atom Initiated Oxidation of Cyclopentane, as a Function
of Temperature and O2 Concentration, in the Presence and
a
Absence of NOx
Firm conclusions regarding the energetics of cyclopentoxy
radical ring-opening are more difficult to obtain, owing to the
dominance of the ring-opening over the O2 reaction, and thus
the difficulty in obtaining definitive temperature-dependent
values for the rate coefficient ratio, k17/k18. Further complications
arise from the possible influence of chemical activation effects21-24
in the chemistry of the cyclopentoxy species. Approximate
Arrhenius parameters for the ring-opening reaction can be
estimated from our low-temperature data, however, under the
initial assumption that the degree of decomposition due to
chemical activation is minimal. The data presented in Table 1
indicate that for conditions of high O2 (500 Torr) and low
temperature (230 K), the decomposition reaction rate still
exceeds that of reaction with O2 by about an order of magnitude,
and thus must be of order 1 × 106 s-1. Assuming an A-factor
of about 1 × 1013 s-1, as was obtained for the cyclohexoxy
ring-opening reaction, leads to an energy barrier to ring-opening
for the cyclopentoxy radical of about 7-8 kcal/mol. Assuming
a higher A-factor, 2 × 1014 s-1 as suggested by Atkinson,18
leads to an activation energy of about 9 kcal/mol. Even with a
very high (70%) occurrence of cyclopentoxy decomposition by
chemical activation, these barrier estimates would only increase
by about 1 kcal/mol. Thus, even the highest probable de-
composition barrier implied by the data obtained in our study
(10 kcal/mol) falls somewhat below the 11-12 kcal/mol that
is obtained using the estimation methods outlined above. The
data obtained regarding the thermodynamics of the cyclopentoxy
radical chemistry support the general conclusion alluded to
above, that decomposition barriers and A-factors for alkoxy
radical decomposition reactions are lower than previously
believed.
with NOx present
no NOx
temp
cyclopentanone cyclopentanone
(K) cyclopentanone CO (100 Torr O2)
(500 Torr O2) CO2
230
240
250
260
300
10
10
11
17
28
7
2.9
2
0.7
<0.5
11
5.5
5
1.7
<0.5
9
9
11
12
11
42
25
10
a Yields were independent of O2, unless otherwise indicated.
measured was 11%, at 230 K and an O2 partial pressure of 500
Torr. The observation of only small yields of cyclopentanone
under these conditions indicates that reaction with O2 (R18) is
of only minor importance in the chemistry of cyclopentoxy
radicals throughout the entire range of conditions present in the
troposphere. Yields of CO were found to decrease with
decreasing temperature (see Table 1), from a value of about
30% at room temperature to values near 10% at 230-240 K.
The decreasing CO yield may result from a decrease in the rate
of the isomerization of the HC(O)CH2CH2CH2CH2O radical
(reaction B of Scheme 2) relative to its reaction with O2 (reaction
A), and/or to an increase in the rate of reaction (E) relative to
that of reaction (D).
Discussion
The data presented above show that, at ambient temperature,
the chemistry of the cyclohexoxy radical is characterized by a
competition between reaction with O2 and ring-opening. Because
of the fairly substantial barrier to ring opening (about 12 kcal/
mol), the importance of this process decreases rapidly with
temperature, such that the O2 reaction will dominate the
atmospheric chemistry of cyclohexoxy at temperatures below
about 270 K. In contrast, the dominant fate of the cyclopentoxy
radical at all temperatures relevant to atmospheric chemistry
will be ring-opening. As first discussed by Takagi et al.,3 the
added ring strain in the C5 system lowers the enthalpy of the
ring-opening, leading to an approximate 100-fold increase in
the rate coefficient for cyclopentoxy ring-opening compared to
that for cyclohexoxy.
Methods for the estimation of the rate coefficients for the
various reactions of alkoxy radicals (reaction with O2, decom-
positions, and isomerizations) have been developed by Atkinson
and co-workers.11,18,26,27 For decomposition reactions, rate
coefficient estimates are obtained by first assuming an A-factor
of 2 × 1014 s-1, multiplied by the reaction degeneracy. The
activation energy (Ed, in kcal/mol) is then estimated from the
following formula: Ed ) (2.4*IP - 8.1) + 0.36∆Hd, where IP
is the ionization potential of the leaving group (in eV), and ∆Hd
is the enthalpy of the decomposition (in kcal/mol). Using this
methodology for the cyclohexoxy radical leads to an Arrhenius
expression for (R5) of k5 ) 4 × 1014 exp(-6730/T) s-1, which
can be compared to our experimentally determined value of
k5 ) 1.2 × 1013 exp (-5750/T) s-1. Over the temperature range
covered by our experiments (260-300 K), the two expressions
agree very well, generating values for k5 that agree to within
20% (approximately the uncertainty in our experimental data).
However, the data obtained herein open up the possibility that
the cyclohexoxy ring-opening process is characterized by a
lower A-factor and lower energy barrier than previously
believed. Similarly low A-factors (≈1013 s-1), with activation
Conclusions
The Cl-atom oxidation of cyclohexane and cyclopentane have
been studied over a range of conditions relevant to atmospheric
chemistry. The chemistry of the cyclohexoxy radical is governed
by a competition between reaction with O2 (R6) and ring-
opening (R5), with k6/k5 ) (1.3 ( 0.3) × 10-27 exp (5550 (
1100/T) cm3 molecule-1. Reaction with O2 will dominate the
chemistry at the temperatures encountered in the middle to upper
troposphere. In contrast, ring-opening is the major fate of the
cyclopentoxy radical under all conditions relevant to the
troposphere. The energy barrier to ring-opening for the cyclo-
pentoxy radicals, < 10 kcal/mol, and possibly for the cyclo-
hexoxy radical as well, are lower than values currently estimated.
Acknowledgment. The National Center for Atmospheric
Research is operated by the University Corporation for Atmo-
spheric Research under the sponsorship of the National Science
Foundation. A portion of this work was supported by the NASA
Upper Atmosphere Research Program. Thanks are due to Frank
Flocke and Alan Fried of NCAR for helpful comments on the
manuscript, and to Karen Henning for assistance in conducting
some of the experiments.
References and Notes
(1) Singh, H. B.; Zimmerman, P. R. Atmospheric Distribution and
Sources of Nonmethane Hydrocarbons. In Gaseous Pollutants: Charac-
terization and Cycling; Nriagu, J. O., Ed.; John Wiley: New York, 1992;
pp 177-235.
(2) Harley, R. A.; Cass, G. R. Atmos. EnViron. 1995, 29, 905.