4.7 Article

Direct time delay computation applied to the O + O2 exchange reaction at low energy: Lifetime spectrum of O3*species

Journal

JOURNAL OF CHEMICAL PHYSICS
Volume 154, Issue 10, Pages -

Publisher

AMER INST PHYSICS
DOI: 10.1063/5.0040717

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It is essential to conduct calculations with nonzero values of the angular momentum quantum number J in order to properly analyze the resonances and time delays of scattering lifetimes in the intermediate heavy ozone complex (50)O3*. The eigenlifetimes show a tendency to increase with J, reaching unusually large values for J = 30, indicating a dense forest of O3* species at higher energies. Conversely, at lower energies and with J=0, the O3* species appear sparse and isolated among overlapping resonances that are not long-lived enough to be considered genuine metastable states.
We report full quantum dynamical calculations for lifetimes of scattering resonances, among which are true metastable states, of the intermediate heavy ozone complex (50)O3* of the O-18 + (OO)-O-16-O-16 reaction, for any value of the total angular momentum quantum number J. We show that computations for nonzero values of J are mandatory in order to properly analyze resonances and time delays, with a view to establish a somewhat comprehensive eigenlife spectrum of the complex O3*. Calculations have been performed in a given low to moderate energy range, including the interval between zero-point energies (ZPEs) of reagents and product species. Quasi-bound states tend to be more numerous, and eigenlifetimes themselves are seen to increase with J, reaching unusually large values for J = 30. A very dense forest of O3* species is pictured already for J greater than 20, especially at the highest energies considered, leading to a quasi-continuum of metastable states. On the contrary, they appear as rather sparse and isolated at J = 0 and lower energies, including the domain between (OO)-O-18-O-16 and (OO)-O-16-O-16 ZPEs, embedded among many overlapping resonances that turn out to be not long-lived enough to be associated with genuine metastable states.

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