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- W2034658075 abstract "An analysis of the possible dissociation of metastable oxygen molecules subject to constraints imposed by selection rules for molecular transitions, airglow observations, and atmospheric chemistry leads to the following conclusions. Dissociation of O 2 ( b 1 ∑ g + ) must produce a negligible number of oxygen atoms at all altitudes in the earth's atmosphere. However, if the dissociation cross section of O 2 ( a 1 Δ g ) has a maximum value in the range 10 −20 cm 2 to 10 −19 cm 2 , then the process O 2 ( a 1 Δ g ) + h ν → O 2 ( C 3 Δ u ) → O( 3 P ) + O( 3 P ) will constitute a significant, and potentially the major, source of odd oxygen in the uppermost stratosphere and mesosphere." @default.
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- W2034658075 title "Dissociation of metastable O<sub>2</sub>as a potential source of atmospheric odd oxygen" @default.
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