GAS-PHASE OZONOLYSIS
403
resulting from the stopped-flow experiments were
chosen. The resulting rate coefficients are (T = 295
0.5 K, unit: cm3 molecule 1 s 1): ␣-pinene: (1.1 0.2)
13. Atkinson, R.; Hasegawa, D.; Aschmann, S. M. Int J
Chem Kinet 1990, 22, 871.
14. Shu, Y.; Atkinson, R. Int J Chem Kinet 1994, 26, 1193.
15. Khamaganov, V. G.; Hites, R. A. J Phys Chem 2001,
105, 815.
16. Kroll, J. H.; Clarke, J. S.; Donahue, N. M.; Anderson, J.
G.; Demerjian, K. L. J Phys Chem 2001, 105, 1554.
17. Kroll, J. H.; Sahay, S. R.; Anderson, J. G.; Demerjian,
K. L.; Donahue, N. M. J Phys Chem 2001, 105, 4446.
18. Molina, L. T.; Molina, M. J. J Geophys Res 1986, 91,
14501.
3
10 16, 1-carene: (5.9 1.0) 10 17, limonene:
16
(2.5 0.3) 10 16, myrcene: (4.8 0.6) 10
,
trans-ocimene:(5.5 0.8) 10 16, terpinolene:(1.6
14
0.4) 10 15, and ␣-terpinene: (1.5
0.4)
10
.
Generally, the presented set of rate coefficients for a
series of terpenes can help to evaluate existing data
and improve the reliability of recommended data.
19. Calvert, J. G.; Atkinson, R.; Kerr, J. A.; Madronich, S.;
Moortgat, G. K.; Wallington, T. J.; Yarwood, G. The
Mechanism of Atmospheric Oxidation of the Alkenes;
Oxford University Press: New York, 2000.
20. Stoer, J.; Bulirsch, R. Einfu¨hrung in die Numerische
Mathematik II; Springer-Verlag: Berlin, 1978.
21. Atkinson, R. Chem Rev 1986, 86, 69.
22. Grosjean, E.; Grosjean, D. Environ Sci Technol 1996,
30, 859.
The authors thank Thomas Conrath and Herwig
Macholeth for technical assistance.
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