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Acknowledgment. Financial support by the Atmospheric
Sciences Division of the National Science Foundation, Grant
No. ATM-9321660, is grateful acknowledged. We are also
grateful to the National Science Foundation for a grant through
the International Program Office, Grant No. INT-9208271.
(10) Schmeisser, M. Inorg. Synth. 1967, 9, 127.
(11) Unless stated otherwise, all thermochemical information has been
taken or derived from the following. (a) Lias, S. G.; Bartness, J. E.; Liebman,
J. F.; Holmes, J. L.; Levin, R. D.; Mallard, W. G. J. Phys. Chem. Ref.
Data, Suppl. 1 1988, 17. (b) Keesee, R. G.; Castleman, A. W., Jr. J. Phys.
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(14) The calculations employ classical RRK theory (Chemical Kinetics
and Dynamics; Steinfeld, J. L., Francisco, J. D., Hase, W. L., Eds.; Prentice-
Hall: Englewood Cliffs, NJ, 1989; p 358) for the prediction of the lifetime,
t ) 1/k, against unimolecular decomposition of the excited NO3-‚(D2O)n,
where the value of the internal energy, E, of these species was taken as
that estimated from the distribution of the exothermicity between ionic,
NO3-‚(D2O)n, and neutral products of reaction 4. The critical energy for
the decomposition process, E°, was taken as being equal to the bond
dissociation energy D[NO3-‚(D2O)n-1-D2O].
(15) (a) Davidson, J. A.; Fehsenfeld, F. C.; Howard, C. J. Int. J. Chem.
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