4230 J. Phys. Chem. A, Vol. 114, No. 12, 2010
Takahashi et al.
and Aschmann,33 Wallington et al.,34 Kaiser and Wallington,24
Stutz et al.,35 and Yamanaka et al.27 There is no discernible
difference between the data obtained in N2 and that in air. The
dependence of k9 on total pressure in the range 700-760 Torr
is negligible. Atkinson and Aschmann,33 Wallington et al.,34
Kaiser and Wallington,24 Stutz et al.,35 and Yamanaka et al.27
report k9/k(Cl + n-C4H10) ) 1.24 ( 0.04, k9/k(Cl + n-C4H10)
) 1.433 ( 0.060, k9/k(Cl + C2H6) ) 4.54 ( 0.21, k9/k(Cl +
n-C4H10) ) 1.1 ( 0.1, and k9/k(Cl + C2H4) ) 2.87 ( 0.14,
respectively. Using k(Cl + n-C4H10) ) 2.05 × 10-10, k(Cl +
C2H6) ) 5.9 × 10-11, and k(Cl + C2H4) ) 9.29 × 10-11 cm3
TABLE 3: Major Reactions in the Cl-Initiated Oxidation of
MBO
addition to terminal carbona
(CH3)2C(OH)CHdCH2 + Cl(+M) f (CH3)2C(OH)CHCH2Cl(+M)
(CH3)2C(OH)CHCH2Cl + O2(+M) f
(CH3)2C(OH)CH(OO·)CH2Cl(+M)
(CH3)2C(OH)CH(OO·)CH2Cl + RO2 f
(CH3)2C(OH)CH(O·)CH2Cl + RO + O2
molecule-1 s-1 20,22
,
gives k9 ) (2.54 ( 0.08) × 10-10, (2.94 (
(CH3)2C(OH)CH(O·)CH2Cl f (CH3)2C(OH) + ClCH2CHO
(CH3)2C(OH) + O2 f (CH3)2CO + HO2
(CH3)2C(OH)CH(O·)CH2Cl f CH2Cl + (CH3)2C(OH)CHO
CH2Cl(+O2) f CH2ClOO(+M)
0.12) × 10-10, (2.68 ( 0.12) × 10-10, (2.26 ( 0.21) × 10-10
,
and (2.67 ( 0.13) × 10-10 cm3 molecule-1 s-1. We estimate
that uncertainties in the reference rate coefficients contribute
an additional 10% uncertainty range. An average of the
determinations of Atkinson and Aschmann,33 Wallington et al.,34
Kaiser and Wallington,24 Stutz et al.,35 and Yamanaka et al.27
CH2ClOO + RO2 f CH2ClO + RO + O2
CH2ClO + O2 f HC(O)Cl+HO2
gives k9 ) 2.62 × 10-10 cm3 molecule-1 s-1
.
Acknowledgment. This study was partly supported by
Program for Improvement of Research Environment for Young
Researchers from Special Coordination Funds for Promoting
Science and Technology (SCF) commissioned by the Ministry
of Education, Culture, Sport, Science and Technology (MEXT)
of Japan (K.T.). This work was also supported in part by Grant-
in-Aids from the MEXT for Scientific Research on Innovative
Areas “Impacts of Aerosols in East Asia on Plants and Human
Health”.
hydrogen abstraction
(CH3)2C(OH)-CHdCH2 + Cl f (·CH2)(CH3)C(OH)-
CHdCH2 + HCl
(·CH2)(CH3)C(OH)-CHdCH2 + O2(+M) f
(·OOCH2)(CH3)C(OH)-CHdCH2(+M)
(·OOCH2)(CH3)C(OH)-CHdCH2 + RO2 f
(·OCH2)(CH3)C(OH)-CHdCH2 + RO + O2
References and Notes
(·OCH2)(CH3)C(OH)-CHdCH2 f HCHO + (CH3)C(OH)-
CHdCH2
(1) Fehsenfeld, F.; Calvert, J.; Fall, R.; Goldan, P.; Guenther, A. B.;
Hewitt, C. N.; Lamb, B.; Liu, S.; Trainer, M.; Westberg, H.; Zimmerman,
P. Global Biogeochem. Cycles 1992, 6, 1389.
(2) Chameides, W.; Lindsay, R.; Richardson, J.; Kiang, C. Science
1988, 241, 1473–1475.
(3) Steiner, A. L.; Tonse, S.; Cohen, R. C.; Goldstein, A. H.; Harley,
R. A. Geophys. Res. Lett. 2007, 34, L15806 DOI:10.1029/2007GL030802.
(4) Goldan, P. D.; Kuster, W. C.; Fehsenfeld, F. C.; Montzka, S. A.
Geophys. Res. Lett. 1993, 20, 1039.
(5) Schade, G. W.; Goldstein, A. H.; Gray, D. W.; Lerdau, M. T. Atmos.
EnViron. 2000, 34, 3535.
(6) Tarvainen, V.; Hakola, H.; Helle´n, H.; Ba¨ck, J.; Hari, P.; Kulmala,
M. Atmos. Chem. Phys. 2005, 5, 989.
(7) Wingenter, O. W.; Kubo, M. K.; Blake, N. J.; Smith, T. W., Jr.;
Blake, D. R.; Rowland, F. S. J. Geophys. Res. 1996, 101, 4331.
(8) Aranda, A.; Mart´ınez, E.; D´ıaz de Mera, Y.; Rodr´ıguez, A.;
Rodr´ıguez, D.; Cuartero, J. Atmos. EnViron. 2003, 37, 4361.
(9) Rodr´ıguez, A.; Rodr´ıguez, D.; Soto, A.; Notario, A.; Aranda, A.;
D´ıaz-de-Mera, Y.; Bravo, I. Atmos. EnViron. 2007, 41, 4693.
(10) Ferronato, C.; Orlando, J. J.; Tyndall, G. S. J. Geophys. Res. 1998,
D103, 25579.
(CH3)C(OH)-CHdCH2 + O2 f CH3C(O)-CHdCH2 + HO2
a Observed products are indicated in bold.
ketone (yield <3%) which, as indicated in Table 3, is an expected
coproduct of HCHO.
The observation of a small yield of glycolaldehyde
(HOCH2CHO) product is of particular interest as it indicates
the formation of OH radicals that are known to react with MBO
to give HOCH2CHO.10 Peroxy and HO2 radicals are formed
during the chlorine atom initiated oxidation of MBO. It has been
shown recently that the reactions of oxygenated peroxy radicals
with HO2 radicals can generate OH radicals.30–32 The observation
of small amounts of glycolaldehyde shows that such reactions
occur during the chlorine-atom-initiated oxidation of MBO.
(11) Fantechi, G.; Jensen, N. R.; Hjorth, J.; Peeters, J. Int. J. Chem.
Kinet 1998, 30, 584.
(12) Takahashi, K.; Iwasaki, E.; Matsumi, Y.; Wallington, T. J. J. Phys.
Chem. A 2007, 111, 1271.
5. Conclusions
(13) Sander, S. P.; Friedl, R. R.; Golden, D. M.; Kurylo, M. J.; Moortgat,
G. K.; Keller-Rudek, H.; Wine, P. H.; Ravishankara, A. R.; Kolb, C. E.;
Molina, M. J.; Finlayson-Pitts, B. J.; Huie, R. E.; Orkin, V. L. Chemical
Kinetics and Photochemical Data for Use in Atmospheric Studies 2006Evalu-
ation No. 15, JPL Publication 06-2.
A large body of self-consistent kinetic and mechanistic data
are provided for the reactions of chlorine atoms with allyl
alcohol, 3-buten-2-ol, and MBO. The data serve to significantly
improve our understanding of the kinetics and mechanism of
the reaction of chlorine atoms with small unsaturated alcohols
of atmospheric importance.
(14) Hilbig, R.; Wallenstein, R. IEEE J. Quantum Electron. 1983, QE-
19, 1759.
(15) Wallington, T. J.; Japar, S. M. J. Atmos. Chem. 1989, 9, 399.
(16) Okabe, H. Photochemistry of Small Molecules; John Wiley and
Sons: New York, 1978.
(17) Matsumi, Y.; Tonokura, K.; Kawasaki, M. J. Chem. Phys. 1992,
97, 1065.
(18) Zare, R. N.; Herschbach, D. R. Proc. IEEE 1963, 51, 173.
(19) Xing, J.-H.; Takahashi, K.; Hurley, M. D.; Wallington, T. J. Chem.
Phys. Lett. 2009, 472, 39–43.
(20) Wallington, T. J.; Andino, J. M.; Lorkovic, I. M.; Kaiser, E. W.;
Marston, G. J. Phys. Chem. 1990, 94, 3644.
Appendix
Justification of the Choice of the Rate Coefficient for the
Cl + C3H6 Reaction, k9, at 700 Torr and 295 K
The kinetics of the reaction of Cl atoms with C3H6 in 700-760
Torr total pressure of N2 or air have been studied by Atkinson