Ozone and TFA Impacts in North America from Degradation of 2,3,3,3-Tetrafluoropropene (HFO-1234yf), A Potential Greenhouse Gas Replacement

We use a regional-scale, three-dimensional atmospheric model to evaluate U.S. air quality effects that would result from replacing HFC-134a in automobile air conditioners in the U.S. with HFO-1234yf. Although HFO-1234yf produces tropospheric ozone, the incremental amount is small, averaging less tha...

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Published inEnvironmental science & technology Vol. 44; no. 1; pp. 343 - 348
Main Authors Luecken, Deborah J, Waterland, Robert L, Papasavva, Stella, Taddonio, Kristen N, Hutzell, William T, Rugh, John P, Andersen, Stephen O
Format Journal Article
LanguageEnglish
Published Washington, DC American Chemical Society 01.01.2010
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ISSN0013-936X
1520-5851
DOI10.1021/es902481f

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Summary:We use a regional-scale, three-dimensional atmospheric model to evaluate U.S. air quality effects that would result from replacing HFC-134a in automobile air conditioners in the U.S. with HFO-1234yf. Although HFO-1234yf produces tropospheric ozone, the incremental amount is small, averaging less than 0.01% of total ozone formed during the simulation. We show that this production of ozone could be compensated for by a modest improvement in air conditioner efficiency. Atmospheric decomposition of HFO-1234yf produces trifluoroacetic acid (TFA), which is subject to wet and dry deposition. Deposition and concentrations of TFA are spatially variable due to HFO-1234yf’s short atmospheric lifetime, with more localized peaks and less global transport when compared to HFC-134a. Over the 2.5 month simulation, deposition of TFA in the continental U.S. from mobile air conditioners averages 0.24 kg km−2, substantially higher than previous estimates from all sources of current hydrofluorocarbons. Automobile air conditioning HFO-1234yf emissions are predicted to produce concentrations of TFA in Eastern U.S. rainfall at least double the values currently observed from all sources, natural and man-made. Our model predicts peak concentrations in rainfall of 1264 ng L−1, a level that is 80× lower than the lowest level considered safe for the most sensitive aquatic organisms.
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ISSN:0013-936X
1520-5851
DOI:10.1021/es902481f