Studies on the production of O2(a1Δg,υ= 0) and O2(b1Σg+,υ= 0) from collisional removal of O2(A3Σu+,υ′ = 6-10)

Author:

Pejaković Dušan A.1,Copeland Richard A.1,Cosby Philip C.1,Slanger Tom G.1

Affiliation:

1. Molecular Physics Laboratory; SRI International; Menlo Park California USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference65 articles.

1. The formation of O2 (a1Δg) in homogeneous and heterogeneous atom recombination;Ali;Can. J. Phys.,1986

2. A new source of ozone in the terrestrial upper atmosphere?;Allen;J. Geophys. Res.,1986

3. Temperature dependence of the collisional removal of O2 (a1Δg, b1Σg+, and c1Σu−) molecules in highly vibrationally excited levels;Amaral;Eos Trans. AGU,2002

4. Excitation and quenching of the oxygen bands in the nightglow;Bates;Planet. Space Sci.,1988

5. The yield of O2 (b1Σg+, υ = 0) produced by quenching of O2 (A3Σg+, υ = 8) by O2;Bednarek;Chem. Phys.,1994

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