Rate Coefficients of O(3P) + HCl at High T
J. Phys. Chem. A, Vol. 106, No. 43, 2002 10237
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mechanical calculations17,21,26 with the J-shifting approximation
(QM/JS)56 based on either the KSG or the S4 PES appear to
agree with experimental data better than quasi-classical trajectory
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5. Conclusions
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Rate coefficients of the reaction O(3P) + HCl in the
temperature range 1093-3197 K were determined using a
diaphragmless shock tube with atomic resonance absorption
detection of O atoms. Our results are consistent with previous
measurements with T < 1486 K but show a steep increase in
the rate coefficients for T > 2000 K. Rate coefficients fit
well with the equation k1(T) ) (9.27 ( 0.03) × 10-24T 3.67(0.18
exp[-(1030 ( 160)/T] cm3 molecule-1 s-1, in which the listed
errors represent one standard deviation. Theoretical calculations
indicate that the reaction path leading to the formation of H +
ClO is unimportant and that two channels lead to the formation
of OH + Cl; the major contribution stems from the channel
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involving TS1 with the smallest barrier, 9.63 kcal mol-1
.
Calculated rate coefficients fit well with experimental observa-
tions throughout the temperature range of investigation.
Acknowledgment. We thank Professors H. Matsui and A.
Tezaki for providing the driver of the shock tube and for helping
us to set up the shock-tube system and Professor D. Truhlar for
the use of the Polyrate program. Y.-P.L. thanks the National
Science Council of Taiwan (grant nos. NSC89-2119-M-007-
001 and NSC89-2113-M-009-010) for support. M.C.L. thanks
the Office of Naval Research, US Navy (contract no. N00014-
89-J1949) for support and the National Science Council of
Taiwan for the distinguished visiting professorship.
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