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024 7 _ |2 pmid
|a pmid:19240934
024 7 _ |2 DOI
|a 10.1039/B814373K
024 7 _ |2 WOS
|a WOS:000263837200012
024 7 _ |2 ISSN
|a 1463-9076
037 _ _ |a PreJuSER-2552
041 _ _ |a eng
082 _ _ |a 540
084 _ _ |2 WoS
|a Chemistry, Physical
084 _ _ |2 WoS
|a Physics, Atomic, Molecular & Chemical
100 1 _ |a von Hobe, M.
|b 0
|u FZJ
|0 P:(DE-Juel1)VDB14301
245 _ _ |a The UV/Vis absorption spectrum of matrix isolated dichlorine peroxide, ClOOCl
260 _ _ |c 2009
|a Cambridge
|b RSC Publ.
300 _ _ |a 1571 - 1580
336 7 _ |a Journal Article
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440 _ 0 |a Physical Chemistry Chemical Physics
|x 1463-9076
|0 4916
|y 10
|v 114
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a UV/Vis absorption spectra of ClOOCl isolated in neon matrices were measured in the wavelength range 220-400 nm. The purity of the trapped samples was checked by infrared and UV/Vis matrix spectroscopy as well as low-temperature Raman spectroscopy. At wavelengths below 290 nm, the results agree with the UV spectrum recently published by Pope et al. [J. Phys. Chem. A, 2007, 111, 4322-4332]. However, the observed absorption in the long wavelength tail of the spectrum-relevant for polar stratospheric ozone loss-is substantially higher than reported by Pope et al. Our results suggest the existence of a ClOOCl electronic state manifold leading to an absorption band similar to those of the near UV spectrum of Cl(2). The differences to previous studies can be accounted for quantitatively by contributions to the reported absorption spectra caused by impurities. The observed band in the long wavelength tail is supported by several high-level ab initio calculations. However, questions arise concerning absolute values of the ClOOCl cross sections, an issue that needs to be revisited in future studies. With calculated photolysis rates based on our spectrum scaled to previous cross sections at the peak absorption, the known polar catalytic ozone-destruction cycles to a large extent account for the observed ozone depletion in the spring polar stratosphere.
536 _ _ |a Atmosphäre und Klima
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650 _ 7 |a J
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700 1 _ |a Stroh, F.
|b 1
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700 1 _ |a Beckers, H.
|b 2
|0 P:(DE-HGF)0
700 1 _ |a Benter, T.
|b 3
|0 P:(DE-HGF)0
700 1 _ |a Willner, H.
|b 4
|0 P:(DE-HGF)0
773 _ _ |0 PERI:(DE-600)1476244-4
|a 10.1039/b814373k
|g Vol. 11, p. 1571 - 1580
|p 1571 - 1580
|q 11<1571 - 1580
|t Physical Chemistry Chemical Physics
|v 11
|x 1463-9076
|y 2009
856 7 _ |u http://dx.doi.org/10.1039/B814373K
909 C O |o oai:juser.fz-juelich.de:2552
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913 1 _ |k P22
|v Atmosphäre und Klima
|l Atmosphäre und Klima
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914 1 _ |y 2009
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|d 30.09.2010
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