Structures and vibrational frequencies of NaO3 and NaO3+: the ionization energy of NaO3
Structures and vibrational frequencies of NaO3 and NaO3+: the ionization energy of NaO3
We use high-level ab initio, up to RCCSD(T), and the density functional theory (DFT) method, B3LYP, to obtain the geometry, vibrational frequencies, and heats of formation of NaO3(X~2B1) and NaO3+(X~1A1). In both cases, a C-2v, diamond structure is deduced. These values allow us also to derive the adiabatic ionization energy. We obtain the following values: ΔHf[NaO3,0K] = -13 ± 2 kcal mol-1, ΔHf[NaO3+,0K] = 167 ± 2 kcal mol-1, and AIE(NaO3) = 7.80 ± 0.05 eV. In addition, it was found that the B3LYP functional performs very well for the O3- species: both geometry and vibrational frequencies. For O3, the method performed well for the geometry, but not so well for the vibrational frequencies. Comparison is made where appropriate to experimental data and to previous calculations. Finally, ΔHr is calculated for a range of reactions that may contribute to the formation of NaO3 or NaO3+ in the atmosphere.
anharmonic potential function, upper-atmosphere, argon matrix, ab-initio, photoelectron-spectroscopy, infrared-spectra, meteoricmetals, ozonide anion, force-field, basis-set
4792-4798
Lee, Edmond P.F.
f47c6d5d-2d1f-4f03-a3ff-03658812d80b
Wright, Timothy G.
20c2bf2d-6181-4571-9fdc-af171ad62cd5
27 May 2004
Lee, Edmond P.F.
f47c6d5d-2d1f-4f03-a3ff-03658812d80b
Wright, Timothy G.
20c2bf2d-6181-4571-9fdc-af171ad62cd5
Lee, Edmond P.F. and Wright, Timothy G.
(2004)
Structures and vibrational frequencies of NaO3 and NaO3+: the ionization energy of NaO3.
Journal of Physical Chemistry A, 108 (21), .
(doi:10.1021/jp0490655).
Abstract
We use high-level ab initio, up to RCCSD(T), and the density functional theory (DFT) method, B3LYP, to obtain the geometry, vibrational frequencies, and heats of formation of NaO3(X~2B1) and NaO3+(X~1A1). In both cases, a C-2v, diamond structure is deduced. These values allow us also to derive the adiabatic ionization energy. We obtain the following values: ΔHf[NaO3,0K] = -13 ± 2 kcal mol-1, ΔHf[NaO3+,0K] = 167 ± 2 kcal mol-1, and AIE(NaO3) = 7.80 ± 0.05 eV. In addition, it was found that the B3LYP functional performs very well for the O3- species: both geometry and vibrational frequencies. For O3, the method performed well for the geometry, but not so well for the vibrational frequencies. Comparison is made where appropriate to experimental data and to previous calculations. Finally, ΔHr is calculated for a range of reactions that may contribute to the formation of NaO3 or NaO3+ in the atmosphere.
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Published date: 27 May 2004
Keywords:
anharmonic potential function, upper-atmosphere, argon matrix, ab-initio, photoelectron-spectroscopy, infrared-spectra, meteoricmetals, ozonide anion, force-field, basis-set
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Local EPrints ID: 20266
URI: http://eprints.soton.ac.uk/id/eprint/20266
ISSN: 1089-5639
PURE UUID: b0e5aa1c-8cf1-4946-88f2-c4d33386d62f
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Date deposited: 20 Feb 2006
Last modified: 15 Mar 2024 06:23
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Author:
Edmond P.F. Lee
Author:
Timothy G. Wright
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