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Does Ozone–Water Complex Produce Additional OH Radicals in the Atmosphere?
Author(s) -
Bing Jin,
Man-Nung Su,
Jim J. Lin
Publication year - 2012
Publication title -
the journal of physical chemistry a
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.756
H-Index - 235
eISSN - 1520-5215
pISSN - 1089-5639
DOI - 10.1021/jp309811n
Subject(s) - ozone , radical , photodissociation , chemistry , photochemistry , atmosphere (unit) , photoionization , absorption cross section , solvation , absorption (acoustics) , ionization , atmospheric chemistry , ultraviolet , molecule , cross section (physics) , meteorology , materials science , organic chemistry , ion , physics , quantum mechanics , optoelectronics , composite material
Ozone-water complex has been thought to play a role in producing atmospheric OH radicals through its photolysis. Here, we re-examined the absorption cross-section of the ozone-water complex with a new method to tell whether the above speculation is valid. With argon solvation and photoionization by tunable vacuum ultraviolet light, we were able to selectively probe the ozone-water 1:1 complex. The measured cross-section of the complex is only similar to the sum of the cross-sections of ozone and water monomers at 157.6, 248.4, and 308.4 nm. In addition, we did not observe any absorption of the complex at 351.8 nm. The results indicate that the OH production through the photolysis of the ozone-water complex is much slower than previously thought.

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