posted on 2008-12-25, 00:00authored byCora J. Young, Michael D. Hurley, Timothy J. Wallington, Scott A. Mabury
Relative rate techniques were used to study the title reactions and determine rate constants of k(Cl + C4F9CH2CH2I) = (1.25 ± 0.15) × 10−12 and k(OH + C4F9CH2CH2I) = (1.2 ± 0.6) × 10−12 cm3 molecule−1 s−1 in 700 Torr total pressure at 295 K. The fluorotelomer aldehyde (C4F9CH2CHO), perfluorinated aldehyde (C4F9CHO), fluorotelomer acid (C4F9CH2C(O)OH), fluorotelomer peracid (C4F9CH2C(O)OOH), and several perfluorocarboxylic acids were detected by in situ FTIR spectroscopy and offline analysis as products of the chlorine atom initiated oxidation of C4F9CH2CH2I in air. The UV−visible spectra of C4F9CH2CH2I and C2H5Cl were recorded over the range of 200−400 nm. Photolysis of C4F9CH2CH2I gives C4F9CH2CHO as the major observed product. By assumption of a photolysis quantum yield of unity, it was calculated that the atmospheric lifetime of C4F9CH2CH2I is determined by photolysis and is a few days. A mechanism for the atmospheric oxidation of fluorotelomer iodides, (CxF2x+1CH2CH2I, where x = 2, 4, 6,...) is proposed. Atmospheric oxidation of fluorotelomer iodides is a potential source of perfluorocarboxylic acids.