Rate coefficients for the reaction of O(<sup>1</sup>D) with the atmospherically long-lived greenhouse gases NF<sub>3</sub>, SF<sub>5</sub>CF<sub>3</sub>, CHF<sub>3</sub>, C<sub>2</sub>F<sub>6</sub>, c-C<sub>4</sub>F<sub>8</sub>, <i>n</i>-C<sub>5</sub>F<sub>12</sub>, and <i>n</i>-C<sub>6</sub>F<sub>14</sub>

Rate coefficients for the reaction of O(<sup>1</sup>D) with the atmospherically long-lived greenhouse gases NF<sub>3</sub>, SF<sub>5</sub>CF<sub>3</sub>, CHF<sub>3</sub>, C<sub>2</sub>F<sub>6</sub>, c-C<sub>4</sub>F<sub>8</sub>, <i>n</i>-C<sub>5</sub>F<sub>12</sub>, and <i>n</i>-C<sub>6</sub>F<sub>14</sub>

The contribution of atmospherically persistent (long-lived) greenhouse gases to the radiative forcing of Earth has increased over the past several decades. The impact of highly fluorinated, saturated compounds, in particular perfluorinated compounds, on climate change is a concern because of their l...

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Bibliographic Details
Main Authors: B. D. Hall, J. B. Burkholder, M. Baasandorj
Format: Article
Language:English
Published: Copernicus Publications 2012-12-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/12/11753/2012/acp-12-11753-2012.pdf

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http://www.atmos-chem-phys.net/12/11753/2012/acp-12-11753-2012.pdf

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