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Global Climate Change Digest A Guide to Information on Greenhouse Gases and Ozone Depletion Published July 1988 through June 1999
FROM VOLUME 4, NUMBER 1, JANUARY 1991
PROFESSIONAL PUBLICATIONS...
ATMOSPHERIC HALOCARBONS
Item #d91jan40
"Reactions of Hydrofluorocarbons and Hydrochlorofluorocarbons with
the Hydroxyl Radical," D.L. Cooper (Dept. Chem., Univ. Liverpool, POB 147,
Liverpool L69 3BX, UK), N.L. Allan, A. McCulloch, Atmos. Environ., 24A(9),
2417-2419, 1990. Reaction rates for H-atom abstraction are important in
determining the atmospheric residence times of HCFCs and HFCs, regarded as
potential substitutes for fully halogenated CFCs. Reaction rates are reported
and a method is given for predicting unknown rates.
Item #d91jan41
"Laboratory Studies of Some Halogenated Ethanes and Ethers:
Measurements of Rates of Reaction with OH and of Infrared Absorption
Cross-Sections," A.C. Brown (Phys. Chem. Lab., Univ. Oxford., S. Parks Rd.,
Oxford OX1 3QZ, UK), C.E. Canosa-Mas et al., ibid., 2499-2511.
A discharge-flow, resonance-fluorescence technique was used in the
temperature range 230-423 K to measure the reaction rates for potential CFC
substitutes. Measurements are used to calculate ozone and global warming
depletion potentials relative to CFCl3.
Item #d91jan42
"Volatile Organic Compounds in Solfataric Gases," V.A. Isidorov
(Chem. Dept., Leningrad Univ., 198904, Leningrad, USSR), I.G. Zenkevich, B.V.
Ioffe, J. Atmos. Chem., 10(3), 329-340, Apr. 1990.
Data obtained through gas chromatographic analysis of volcanic gas samples
confirm the existence of a natural source of halocarbons that have a long
lifetime in the troposphere. They play an important role in the greenhouse
effect and in the catalytic cycle of destruction of stratospheric ozone.
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