期刊
ATMOSPHERIC ENVIRONMENT
卷 44, 期 9, 页码 1186-1191出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2009.12.026
关键词
Photolysis; Cross-sections; Quantum yields; Greenhouse gas; NF(3)
Although NF(3), a trace gas of purely anthropogenic origin with a large global warming potential is accumulating in the Earth's atmosphere, little photochemical data exists from which to calculate its atmospheric removal rate. In this study, photodissociation quantum yields, Phi(1), were derived following 193.3 nm laser photolysis of NF(3), and quantitative conversion of the F-atom photoproducts to OH, which was detected by laser induced fluorescence. Values of Phi(1)(P, T) = (1.03 +/- 0.05) were determined at pressures between 28 and 100 mBar of He or N(2) and at either room temperature or 255 K. Absorption cross-sections, sigma, obtained between 184 and 226 nm were combined with the values of Phi(1)(P, T) to confirm a long (approximate to 700 year) photolysis lifetime for NF(3). No evidence for reaction of OH with NF(3) was found, indicating that this process makes little or no contribution to NF(3) removal from the atmosphere. These results underpin recent calculations of an NF(3) atmospheric lifetime tau approximate to 550 years, largely controlled by photolysis in the stratosphere. In the course of this work the rate coefficient k(2)(298 K) = (1.3 +/- 0.2) x 10(-11) cm(3) molecule(-1) s(-1) was obtained for the reaction F + H(2)O. (C) 2010 Elsevier Ltd. All rights reserved.
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