Chlorine isotope fractionation in the stratosphere

Laube, JC, Kaiser, J ORCID:, Sturges, WT ORCID:, Bonisch, H and Engel, A (2010) Chlorine isotope fractionation in the stratosphere. Science, 329 (5996). p. 1167. ISSN 1095-9203

Full text not available from this repository. (Request a copy)


Chlorinated organic compounds are important contributors to the anthropogenic enhancement of stratospheric ozone depletion. We report measurements of stratospheric isotope fractionation in such a compound. Stratospheric and tropospheric difluorodichloromethane (CF2Cl2) were found to have the largest relative 37Cl/35Cl isotope ratio difference ever measured for a natural compound. The increase of the relative isotope ratio difference with altitude was tightly correlated to the corresponding decrease in the CF2Cl2 mixing ratio. The observed relationship has a high potential to provide new insights into atmospheric chemistry and transport processes.

Item Type: Article
Uncontrolled Keywords: sdg 12 - responsible consumption and production ,/dk/atira/pure/sustainabledevelopmentgoals/responsible_consumption_and_production
Faculty \ School: Faculty of Science > School of Environmental Sciences
Related URLs:
Depositing User: Rosie Cullington
Date Deposited: 15 Feb 2011 11:58
Last Modified: 23 Oct 2022 01:31
DOI: 10.1126/science.1191809

Actions (login required)

View Item View Item