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products can arise if both SO2 ions and atomic species are
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Conclusions
The rate constants and product-ion branching ratios for the
reactions of SOxFy ions with H, H2, N, N2, NO, and O have
-
been measured in a SIFT. None of the ions reacts with H2, N2,
and NO; thus, the rate constants are <1 × 10-12 cm3 s-1. All
-
-
of the SOxFy ions react with O; however, only SO2 reacts
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with both N and O. The rate constants for SOxFy reactions
with H and O at 298 K are e25% of the collision rate constant
as seen previously for O3 reactions with these ions, consistent
with a kinetic bottleneck that has been found to limit the
reactivity. The only exceptions are the reactions of SO2 with
N and O, which are much more efficient.
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SOxFy- ions react with H solely via fluorine-atom abstraction
to form HF at 298 and 500 K. Successive F-atom removal does
not occur at either temperature, and the rate constants show no
temperature dependence over this limited range. Three pathways
were observed with O atoms: F-atom exchange in the reactant
ion, F- exchange in the reactant ion, and charge transfer to the
O atom. Associative detachment was observed only in the
reactions of SO2- and F- with H atoms. Theoretical calculations
of the HSO2- isomeric structures were performed to understand
the reaction mechanism for detachment. The calculations show
that structural differences between the ionic and neutral HSO2
species can account for the reactivity limitations observed in
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Acknowledgment. We thank Thomas Miller for helpful
discussions and John Williamson and Paul Mundis for technical
support. This work was supported by the Air Force Office of
Scientific Research under Program EP2303A. A.J.M. was
supported through Boston College under Contract FA8718-04-
C-0006.
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