Transition probabilities and Franck-Condon factors for the second negative band system of O sub 2 sup +
Journal Article
·
· Journal of Geophysical Research; (United States)
- State Univ. of New York, Stony Brook (United States)
- Harvard-Smithsonian Center for Astrophysics, Cambridge, MA (United States)
The second negative band system of O{sub 2}{sup +} arises from the transition A{sup 2}II{sub u}({nu}{prime}) {yields} X{sup 2}II{sub g}({nu}{double prime}). The excited electronic state A{sup 2}II{sub u} can be populated by photoionization and electron impact ionization of O{sub 2} and by fluorescent scattering of radiation by O{sub 2}{sup +} (X{sup 2}II{sub g}) in planetary and cometary atmospheres. Transition probabilities for the second negative band system of O{sub 2}{sup +} are computed using the dipole transition moment presented by Wetmore et al. (1984). Vibrational levels {nu}{double prime} = 0-54 of the X{sup 2}II{sub g} ground state and {nu}{prime} = 0-33 of the excited A{sup 2}II{sub u} state are included. Franck-Condon factors for ionization-excitation of O{sub 2} (X{sup 3}{Sigma}{sub g}{sup {minus}}; {nu} = 0-25) to O{sub 2}{sup +}(A{sup 2}II{sub u}; {nu}{prime} = 0-33) are also presented.
- OSTI ID:
- 5133430
- Journal Information:
- Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 95:A2; ISSN 0148-0227; ISSN JGREA
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
640107* -- Astrophysics & Cosmology-- Planetary Phenomena
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
ATMOSPHERES
CALCULATION METHODS
CHARGED PARTICLES
CHEMICAL COMPOSITION
COMETS
ENERGY LEVELS
ENERGY-LEVEL TRANSITIONS
FRANCK-CONDON PRINCIPLE
FUNCTIONS
GROUND STATES
IONS
OXYGEN IONS
PLANETARY ATMOSPHERES
WAVE FUNCTIONS
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
ATMOSPHERES
CALCULATION METHODS
CHARGED PARTICLES
CHEMICAL COMPOSITION
COMETS
ENERGY LEVELS
ENERGY-LEVEL TRANSITIONS
FRANCK-CONDON PRINCIPLE
FUNCTIONS
GROUND STATES
IONS
OXYGEN IONS
PLANETARY ATMOSPHERES
WAVE FUNCTIONS