The photochemical formation of electronically excited oxygen molecules in the atmosphere
作者:
R. P. Wayne,
期刊:
Quarterly Journal of the Royal Meteorological Society
(WILEY Available online 1967)
卷期:
Volume 93,
issue 395
页码: 69-78
ISSN:0035-9009
年代: 1967
DOI:10.1002/qj.49709339506
出版商: John Wiley&Sons, Ltd
数据来源: WILEY
摘要:
AbstractSpectroscopic studies of the airglow indicate that electronically excited molecular oxygen in the1Δgand1Σg+states is produced in the atmosphere. The way in which the excited states are formed in the atmosphere has been the subject of much speculation, and the present paper attempts to evaluate some of the mechanisms proposed in the light of laboratory experiments.The most probable excitation mechanism for O2(1Δg) appears to be the primary step in the photolysis of atmospheric ozone:O3+ hν (λ<3,100 Å) → O2(1Δg) + (1D).O2(1Δg+) may then be formed in the energy‐pooling process:O2(1Δg) + O2(1Δg) → O2(1
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