RESEARCH PAPER a b PCCP Stig R. Sellevåg,a Tanya Kelly,b Howard Sidebottomb and Claus J. Nielsen*a www.rsc.org/pccp A study of the IR and UV-Vis absorption cross-sections, photolysis and OH-initiated oxidation of CF3CHO and CF3CH2CHOy Department of Chemistry, University of Oslo, P.O. Box 1033, Blindern, N-0315 Oslo, Norway. E-mail: [email protected]; Fax: þ47 22 85 54 41; Tel: þ47 22 85 56 80 Department of Chemistry, University College Dublin, Belfield Dublin 4, Ireland Received 9th December 2003, Accepted 27th January 2004 F|rst published as an Advance Article on the web 23rd February 2004 Infrared and ultraviolet-visible absorption cross-sections, effective quantum yields of photolysis and OH reaction rate coefficients for CF3CHO and CF3CH2CHO are reported. Relative rate measurements at 298(2) K and 1013(10) hPa, give k(OH þ CF3CHO)/k(OH þ CH3CH3) ¼ 2.00(13), k(OH þ CF3CH2CHO)/ k(OH þ CH3CH2OH) ¼ 1.21(5) and k(OH þ CF3CH2CHO)/k(OH þ HC(O)OC2H5) ¼ 3.51(9) (2s). The effective quantum yield of photolysis was measured under pseudo-natural conditions in the European simulation chamber, Valencia, Spain (EUPHORE). Over the wavelength range 290–400 nm, the effective quantum yields of photolysis for CF3CHO and CF3CH2CHO are less than 2 102 and 4 102, respectively. The tropospheric lifetimes are estimated to be: tOH(CF3CHO) 26 days; tphotol(CF3CHO) > 27 days; tOH(CF3CH2CHO) 4 days; tphotol(CF3CH2CHO) > 15 days. DOI: 10.1039/b315941h 1. Introduction Partially fluorinated alcohols have been suggested as new replacement compounds for hydrochlorofluorocarbons (HCFCs) and hydrofluorocarbons (HFCs). A number of investigations on the kinetics and mechanism for the atmospheric degradation of CF3CH2OH have been reported.1–5 Trifluoroacetaldehyde (CF3CHO) has been shown to be the primary degradation product in the OH-initiated oxidation of CF3CH2OH.4,5 CF3CHO is also a key intermediate in the atmospheric removal of HFC-143a (CF3CH3).6 Similarly, CF3CH2CHO has been reported as the primary oxidation product of CF3CH2CH2OH.4 In order to obtain a more complete picture of the environmental burden of fluorinated industrial compounds, it is necessary to have information about the atmospheric lifetimes and global warming potentials of the degradation products from the oxidation of the alcohols. This information is deficient for CF3CHO and for CF3CH2CHO no previous studies on OH kinetics or absorption cross-sections in the infrared (IR) and ultraviolet-visible (UV-Vis) regions have been published. A few experimental and theoretical studies of the reaction between OH and CF3CHO are available in the literature. Dóbé et al.7 measured a reaction rate coefficient of 6.7(4.0) 1013 cm3 molecule1 s1 at 299 K by using the discharge flowresonance fluorescence technique. Dóbé et al. reported an activation energy of 5.9 kJ mol1 for this reaction. However, this was based on an estimated pre-exponential factor of 7 1012 cm3 molecule1 s1. Scollard et al.8 reported two values for the OH reaction rate coefficient of CF3CHO: 6.5(5) 1013 and 5.5(1.2) 1013 cm3 molecule1 s1, the former determined from laser photolysis-resonance fluorescence experiments and the latter measured relative to acetone. y Electronic supplementary information (ESI) available: absorption cross-sections of CF3CHO (Table S1), CF3CH2CHO (Table S2), and FACSIMILE kinetic model of the CF3CHO/CH3CH3/O3/H2 reaction system (Table S3). See http://www.rsc.org/suppdata/cp/ b3/b315941h/ From pulsed laser photolysis-resonance fluorescence measurements, Laverdet et al.9 reported an Arrhenius expression equal to 3.5(1.0) 1012exp[488(57) K/T] cm3 molecule1 s1 over the temperature range 233–313 K giving a rate constant of 6.8 1013 cm3 molecule1 s1 at 298 K. As can be seen, there is a relatively large scatter among the results of these studies. Theoretical studies on the OH reaction with CF3CHO have been carried out by Francisco,10 Rayez et al.11,12 and Chandra et al.13 Francisco and Williams14 have measured the infrared absorption intensities of CF3CHO in the wavenumber region 2890–801 cm1. Ultraviolet-visible absorption cross-sections of CF3CHO have been determined by Francisco and Williams,14 Libuda15 and Meller et al.16 The photolysis of CF3CHO was first reported by Dodd and Smith.17 At 313 nm and room temperature, they determined a quantum yield equal to 0.021 for the primary process yielding CHF3 and CO, and a quantum yield of 0.12 for the process yielding CF3 and HCO in the pressure range 40–53 hPa. Pearce and Whytock18 investigated the importance of the molecular channel at the same wavelength, and found a quantum yield within experimental error of zero. Richer et al.19 studied the photolysis of CF3CHO in air at lmax ¼ 253.7 nm and lmax ¼ 366 nm. The product yields at 253.7 nm of CHF3 (14%), CF2O (80%), CO (65%) and CO2 (45%) suggest the molecular channel is significant at this wavelength. However, CF3CHO was reported to undergo only a small degree of dissociation at lmax ¼ 366 nm after more than six hours photolysis. In order to provide better estimates of the atmospheric lifetimes of CF3CHO and CF3CH2CHO, we have measured their OH reaction rate coefficients using the relative rate method. We have also determined their effective quantum yield of photolysis under pseudo-natural conditions at the European simulation chamber, Valencia, Spain (EUPHORE). Finally, measurements of infrared and ultraviolet-visible absorption cross-sections are presented. Based on these data, an assessment of the environmental impact including the radiative forcing and global warming potentials of CF3CHO and CF3CH2CHO is made. This journal is Q The Owner Societies 2004 Phys. Chem. Chem. Phys., 2004, 6, 1243–1252 1243 2. Experimental 2.1. Measurements of IR and UV-Vis absorption cross-sections The absorption cross-section of a compound J at a specific wavenumber n~ is according to Beer–Lambert’s law given by s(~ n ) ¼ Ae(~ n )/nJl, where Ae(~ n ) ¼ ln t(~ n ) is the naperian absorbance, t is the transmittance, nJ is the number density of J and l is the path length where the absorption takes place. The integrated absorption intensity, Sint , is given by: Z sð~ n Þd~ n ðIÞ Sint ¼ Absolute integrated absorption intensities of CF3CHO and CF3CH2CHO were measured at 298(2) K in the region 4000–400 cm1. Three independent experiments were performed. Fourier-transform infrared (FTIR) spectra of the pure vapours were recorded using a Bruker IFS 113v spectrometer employing a nominal resolution of 1.0 cm1 and BlackmanHarris 3-Term apodization of the interferograms. A Ge/KBr beamsplitter was used to cover the spectral region. To ensure optical linearity, a deuterated triglycine sulfate (DTGS) detector was used. Eight single channel spectra each recorded with 32 scans were averaged to yield one background or sample spectrum. A gas cell of 2.34(2) cm length equipped with KBr windows was employed. The partial pressures of the gases were in the range between 1 and 10 hPa, and were measured using an absolute pressure transducer (MKS Baratron Type 122A) with a stated accuracy of 0.15%. Absorption cross-sections in the UV-Vis region were measured at 298(2) K using a Agilent 8453E photodiode array spectrophotometer having a spectral resolution of 2 nm. The spectra were recorded in the wavelength range from 190 nm to 1100 nm at sampling intervals of 1 nm. The integration time was set to 0.5 s. The pressures of the pure vapours were in the range 3 to 95 hPa, and were measured using a MKS Baratron Type 122A pressure transducer. A gas cell of 8.0(1) cm length with quartz windows was used. 2.2. Relative rate measurements In the relative rate method (RR), the reaction rate coefficient for the compound of interest is measured relative to a reference compound with a known rate coefficient. If the reactants react solely with the same radical and the reactants are not regenerated in the system, the relative rate coefficient, krel , is given according to the following expression:20 ½ A 0 ½R0 kA ¼ krel ln ; krel ¼ ln ; ðIIÞ ½ A t ½ R t kR where A is the compound of interest and R is the reference compound. [A]0 , [R]0 , [A]t and [R]t are the concentrations of A and R at the start and at the time t, respectively, and kA and kR are the rate coefficients. The ‘‘ Oslo experiments ’’ were carried out in purified air at 298(2) K and 1013(10) hPa in a 250 L reaction chamber of electro-polished stainless steel with online FTIR detection. The reaction chamber was equipped with White multi-reflection optics and had an optical path length of 120 m. The spectrometer was a Bruker IFS 88 instrument and a mercury–cadmium–telluride (MCT) detector was used. In all experiments, spectra were recorded in the wavenumber range 4500–400 cm1. Each spectrum was recorded by adding 100 scans and employing a resolution of 0.5 cm1 and Happ–Genzel apodization. Typically, it took ca. two minutes to record one spectrum. The initial mixing ratios of the reactants were 2–4 ppm. Hydroxyl radicals were produced in two different ways. In Phys. Chem. Chem. Phys., 2004, 6, 1243–1252 CD3 CHðONOÞCD3 þ hn ! CD3 CHðOÞCD3 þ NO ð1Þ CD3 CHðOÞCD3 þ O2 ! CD3 CðOÞCD3 þ HO2 ð2Þ HO2 þ NO ! OH þ NO2 band 1244 the OH reaction with CF3CH2CHO, hydroxyl radicals were generated by photolysis of 2-propylnitrite-1,1,1,3,3,3-d6 (10– 15 ppm) employing two Philips TLD 18W/08 fluorescence lamps (lmax 375 nm) mounted in a quartz tube inside the reaction chamber. The lamps were turned off during recording of the spectra. Photolysis was carried out in intervals of 1–5 min. The mechanism for OH production from photolysis of 2-propylnitrite-1,1,1,3,3,3-d6 is as follows: ð3Þ 2-Propylnitrite-1,1,1,3,3,3-d6 could not be used as a precursor for OH radicals in the reaction between OH and CF3CHO because this reaction was too slow. Instead, OH radicals were generated by photolysis of O3 in the presence of H2 (reactions (4) and (5)). Ozone was produced by discharge of oxygen, where approximately two percent of the oxygen gas was converted to ozone. Typical mixing ratios of ozone and hydrogen were 3 102 ppm and 5 103 ppm, respectively. O3 þ hnðlmax 310 nmÞ ! Oð1 DÞ þ O2 ð4Þ Oð1 DÞ þ H2 ! OH þ H ð5Þ Photolysis of ozone was carried out in intervals of 1–2 min using two Philips TL 20W/12 fluorescence lamps (lmax 310 nm). Both CF3CHO and CF3CH2CHO were stable in the dark in the reaction chamber. Some surface adsorption of CF3CHO (ca. 3%) was observed for about 15 min after admission to the cell. The aldehydes did not photolyse to any observable degree during the time scale of the kinetic experiments. The ‘‘ Dublin experiments ’’ were performed in a FEP Teflon reaction chamber with a volume of approximately 50 L. All experiments were performed in purified air at atmospheric pressure (973–1013 hPa) and at 298(2) K. Electric fans positioned below the chamber ensured that a uniform temperature was maintained during irradiation of the reaction mixtures. Measured amounts of substrate and reference compounds were flushed from calibrated bulbs into the partly inflated reaction chamber by a stream of zero-grade air. All pressure readings were made using MKS Baratron pressure transducers (Model 122 A). When all the reactants had been added to the chamber it was subsequently filled to maximum capacity at ca. 1 atm pressure and kept in the dark for 1 h to allow complete mixing of the reactants. A homogeneous reaction mixture was confirmed by constant, reproducible gas chromatographic analysis. Hydroxyl radicals were generated by photolysis of ozone in the presence of water vapour using four germicidal lamps (Philips TUV, 15 W): O3 þ hnðlmax 254 nmÞ ! Oð1 DÞ þ O2 ð6Þ Oð1 DÞ þ H2 O ! OH þ OH ð7Þ Ozone was produced by passing zero-grade air through an ozone generator (Monitor Labs) directly into the reaction chamber, at a flow rate of 1 L min1 for 10 min. Triply distilled water was injected directly into the reaction chamber. Mixtures of substrate, reference and O3/H2O were photolysed until about 50% depletion of the substrate or reference compound had occurred. Typical initial concentrations employed were [substrate]0 ¼ [reference]0 ¼ 15–80 ppm, [O3] 50 ppm and [H2O] 2 103 ppm. Quantitative analyses were carried out using gas chromatography (Shimadzu 8A, incorporating a flame ionisation detector). A Valco gas-sampling valve was used to remove samples of the reaction mixtures from the reaction chamber for GC analysis. Photolysis of CF3CH2CHO This journal is Q The Owner Societies 2004 was negligible over the time scale of the kinetic experiments and the aldehyde was stable in the chamber in the dark. 2.3. Experiments performed at EUPHORE A detailed description of the EUPHORE facility and the existing analytical instruments is given by Becker.21 Here, a brief description of the installation is given based on that report. The present photolysis experiments were carried out in a hemispherical outdoor simulation chamber of volume about 200 m3 made of FEP foil with a thickness of 0.127 mm. The FEP foil has a transmission of more than 80% of the solar radiation in the wavelength range between 280 and 640 nm. The chamber was equipped with a Nicolet Magna 550 FTIR spectrometer coupled with a White multi-reflection mirror system for in situ analysis. The optical path length was 553.5 m. FTIR spectra were recorded every ten minutes by adding 900 interferograms with a resolution of 1.0 cm1. The photolysis of CF3CHO and CF3CH2CHO were studied in purified air (see Becker21 for a description of the drying and purification system). The mixing ratios of CF3CHO and CF3CH2CHO in the chamber were ca. 1 ppm. Di-n-butyl ether (DNBE), 0.2 ppm, was added to the reaction chamber as a tracer to monitor the OH radical activity, k(OH þ DNBE) ¼ 2.89 1011 cm3 molecule1 s1.22 The aldehydes may be removed from the chamber by photolysis (8), reaction with OH radicals (9) and leakage (10). The loss of DNBE is solely due to its reaction with OH radicals (11) and to leakage (12). Approximately 20 ppb of SF6 was added to the reaction chamber to determine the leak rate coefficient (reaction (13)), kleak : lnf½SF6 0 =½SF6 t g ¼ kleak t ðIIIÞ where [SF6]0 and [SF6]t are the initial SF6 concentration and that after a time t, respectively. Aldehyde þ hn ! Products J obs ð8Þ Aldehyde þ OH ! Products kald ð9Þ kleak ð10Þ kDNBE ð11Þ Di-n-butyl ether ! Loss by leakage kleak ð12Þ SF6 ! Loss by leakage kleak ð13Þ Aldehyde ! Loss by leakage Di-n-butyl ether þ OH ! Products Thus, it can be shown that the observed photolysis rate coefficient, Jobs , of the aldehydes can be obtained from the expression: ½Ald0 ½DNBE0 kald ln ln ½Aldt kDNBE ½DNBEt kDNBE kald ¼ kleak þ Jobs t ðIVÞ kDNBE From the observed photolysis rate, the effective quantum yield for the photolysis of the aldehyde under study can be calculated according to the following expression: Feff ¼ J obs =J max ðVÞ where the maximum photolysis rate coefficient, Jmax , is given by: Z J max ¼ sðlÞfðlÞF ðlÞdl ðVIÞ Here s(l) is the absorption cross-section (base e) of the aldehyde in units of cm2 molecule1, f(l) is the quantum yield (f(l) ¼ 1) and F(l) is the solar actinic flux (photons cm2 s1). The integration was carried out over the wavelength range 290–400 nm. The actinic flux was calculated from the photolysis rate coefficient of NO2 , J(NO2), and the photolytic production rate coefficient of O(1D), J(O(1D)). The specifications of the J(NO2) and J(O(1D)) radiometers are given by Becker.21 CF3 radicals are formed in the degradation of CF3CHO17,18 and the subsequent reaction with O2 will lead to the generation of CF3O radicals. It is possible that CF3O could react rapidly with CF3CHO and hence, ca. 125 ppm of NO was added to the reaction chamber in order to provide a sink for CF3O radicals:23 CF3 O þ NO ! CF2 O þ FNO 2.4. ð14Þ Chemicals CF3CHO was synthesised by adding 1-ethoxy-2,2,2-trifluoroethanol (Aldrich, 90%) to concentrated sulfuric acid (95%). After ca. one hour mixing, CF3CHO was distilled off under vacuum and trapped in a container at liquid nitrogen temperature. The purity was estimated to be better than 98%. CF3CH2CHO (Fluorochem, > 97%), CH3CH2OH (Aldrich, 96%) and HC(O)OC2H5 (Aldrich, > 97%) were used without further purification. Purified air containing 80% N2 and 20% O2 (CO þ NOx < 100 ppb and CnHm < 1 ppm), oxygen gas (99.95%), hydrogen gas (99%) and ethane (99.0%), used in the relative rate experiments performed in Oslo, were delivered from AGA. In the ‘‘ Dublin experiments ’’, synthetic air was zero-grade from Air Products. The preparation of 2-propylnitrite-1,1,1,3,3,3-d6 from 2-propanol-1,1,1,3,3,3-d6 followed the procedure reported for n-butyl nitrite.24 2-Propanol1,1,1,3,3,3-d6 was prepared from acetone-d6 (Cambridge Isotope Laboratories, Inc., 99.9%) by reduction with NaBH4 in a basic water solution. All organic compounds except ethane, were purified/degassed by three freeze–pump–thaw cycles. 3. Results 3.1. IR and UV-Vis absorption cross-sections In the determination of IR absorption cross-sections, single channel spectra of the empty cell were recorded before and after each sample spectrum. An average of the two transmittance spectra was used in the succeeding analysis. The integrations over the absorption bands were carried out using a method that defines the baseline from an average of two points on one side of the band, and the average of two points on the other side of the band. The integrated absorption intensities of the absorption bands, or regions of overlapping bands, were determined by plotting the integrated absorbance against the product of the number density and the path length. None of the regression lines had a y-intercept significantly different from zero. We therefore used a least-squares method that forced the regression line to go through zero in order to determine the absorption intensities. We have only quantified uncertainties in pressure measurements, path length and temperature as systematic errors. These are 0.15%, 0.90% and 0.67%, respectively, where the uncertainty in path length includes both geometrical and optical errors. The absorption cross-sections (base e) of CF3CHO and CF3CH2CHO in the 4000–400 cm1 region are shown in Fig. 1a and b, respectively, and the integrated absorption intensities are given in Tables 1 and 2, respectively. As can be seen from Table 1, the estimated uncertainty in the total absorption intensity of CF3CHO is less than two percent, and includes error from the least-squares fit and the above-mentioned This journal is Q The Owner Societies 2004 Phys. Chem. Chem. Phys., 2004, 6, 1243–1252 1245 Table 2 Absolute integrated absorption intensities, Sint , of CF3CH2CHO in the mid-infrared region. See text for a discussion on the uncertainties Wavenumber range/cm1 Sint/1017 cm molecule1 585–505 705–595 905–800 1475–915 1850–1675 2950–2650 0.094 0.004 0.220 0.030 0.010 0.008 11.7 0.6 1.77 0.06 0.74 0.11 26% lower. The UV spectrum of CF3CH2CHO (Fig. 2b) is not shifted compared to CH3CH2CHO,25 but again the cross-sections are approximately 26% lower. 3.2. OH reaction rate coefficients Losses of reactant and reference compounds were monitored by FTIR spectroscopy in the ‘‘ Oslo experiments ’’. Spectral subtraction was used to determine the concentrations of the substrate and reference compounds at different time intervals during the relative rate experiments. The relative rate coefficients were determined according to eqn. (II) by a weighted least-squares method that includes uncertainties in the concentrations of both reactants obtained by the spectral subtraction procedure.26 Each relative rate coefficient was determined from three independent measurements. The reported uncertainties in this work represent 2s from the statistical analyses and do not include any systematic errors or uncertainties in the reference Fig. 1 Infrared absorption cross-sections (base e) of pure vapour at 298(2) K of (a) CF3CHO and (b) CF3CH2CHO. systematic errors. For CF3CH2CHO the uncertainty is somewhat larger, most of which we cannot account for. UV-Vis absorption cross-sections of CF3CHO and CF3CH2CHO at 298(2) K were determined from three independent measurements. Their UV-Vis spectra are shown in Fig. 2a and b, respectively. The absorption bands of both aldehydes corresponds to the weak p* n transition of the carbonyl group. At the wavelength of maximum absorption, the uncertainty in the absorption cross-section is 0.5% for CF3CHO and 2.8% for CF3CH2CHO (2s; error from the least-squares fit only). When systematic errors in pressure measurements, temperature, optical path length and instrumental drift also are taken into account, it is estimated that the absolute error limits of the integrated cross-sections are in the order of 5%. The absorption cross-sections of CF3CHO and CF3CH2CHO are given as Electronic Supplementary Information (ESI)y in Tables S1 and S2, respectively. As can be seen from Fig. 2a, the UV spectrum of CF3CHO is red-shifted by approximately 10 nm as compared to CH3CHO.25 Further, the cross-sections are on average ca. Table 1 Absolute integrated absorption intensities, Sint , of CF3CHO in the mid-infrared region. See text for a discussion on the uncertainties 1246 Wavenumber range/cm1 Sint/1017 cm molecule1 600–465 750–670 990–775 1450–1050 1950–1600 3000–2610 0.259 0.006 0.508 0.009 0.617 0.009 10.42 0.12 1.085 0.014 0.614 0.016 Phys. Chem. Chem. Phys., 2004, 6, 1243–1252 Fig. 2 (a) UV-Vis absorption cross-sections (base e) of pure vapour of CF3CHO at 298(2) K: (——) this work; (---) Meller et al.;16 ( ) Libuda;15 (–.– ) Francisco and Williams.14 (b) UV-Vis absorption cross-sections of CF3CH2CHO (pure vapour) at 298(2) K. This journal is Q The Owner Societies 2004 rate coefficients. Based on the residuals in the spectral subtraction, the uncertainty in the relative concentrations of the reactants is estimated to be 1%. The rate coefficient for the reaction OH þ CF3CHO was measured using CH3CH3 as reference compound. The wavenumber region 2950–2700 cm1, i.e., part of the C–H stretching region, was analysed in order to determine the relative concentrations of both CF3CHO and CH3CH3 . FTIR reference spectra of CF3CHO, CH3CH3 , O3 , HCHO, HCOOH (very small amounts) and a sloping baseline were included in the spectral subtractions. An example of the residuals after the spectral subtractions is given in Fig. 3. Fig. 4 shows the decay of CF3CHO versus CH3CH3 in the presence of hydroxyl radicals, plotted according to eqn. (II). From these data a relative rate coefficient of 2.00(13) was extracted. The latest JPL data evaluation27 has recommended a rate coefficient of 2.4 1013 cm3 molecule1 s1 for the reaction between OH and CH3CH3 at 298 K. On an absolute scale, the derived OH reaction rate coefficient of CF3CHO is therefore 4.80(31) 1013 cm3 molecule1 s1. The OH-initiated oxidation of CF3CHO results in generation of CF3O radicals. It is known that CF3O reacts with ethane with a rate coefficient of 1.23 1012 cm3 molecule1 s1.27 The CF3O radicals may therefore react significantly with both CF3CHO and the reference compound. We have assumed the large concentrations of H2 in the system, which was used as the OH source by reaction with O(1D), would act as a scavenger for CF3O radicals. To support this, we modelled the CF3CHO/CH3CH3/O3/H2 reaction system using FACSIMILE.28 Eighty-three reactions were included in the model (see Table S3y for details). Rate coefficient data were taken from the IUPAC,23 NIST29 and JPL27 databases. NOx chemistry have been included in the model together with reactions describing the formation of CH3C(O)O2NO2 (peroxy acetyl nitrite, PAN) and CF3C(O)O2NO2 . However, since the concentration of NOx in the reaction chamber is very low, the model showed that these reactions do not make any significant contribution in describing the ongoing chemistry in the chamber. Some of the key reactions used in the model are given in Table 3. As can be seen, the rate coefficients for the reactions CF3O þ H2 and CF3O þ CF3CHO have been estimated. The estimate of k(CF3O þ H2) is based on the rate coefficient for the reaction CF3O þ CH4 . The reactivity of OH radicals towards H2 is similar to that towards CH4 .23 Assuming that Fig. 4 Decay of CF3CHO versus CH3CH3 in the presence of OH radicals at 298(2) K as measured from three independent experiments. The uncertainty in each data point is based on an estimated uncertainty of 0.01 in the relative concentrations. The uncertainty of the linear regression coefficients y ¼ 0.005(6) þ 1.208(25) represents 1s. this also holds for the CF3O radicals, we have estimated that k(CF3O þ H2) ¼ 2 1014 cm3 molecule1 s1. Similar arguments for the reactivity of CF3O towards CF3CHO versus that towards CH3CH3 justifies the rate coefficient k(CF3O þ CF3CHO) ¼ 3 1012 cm3 molecule1 s1. Based on these estimates and the relative concentrations of H2 , C2H6 and CF3CHO employed in the experiments, the model predicted that the reaction of CF3O with H2 is 10–30 times more frequent than its reactions with CF3CHO and CH3CH3 . Variations in the concentrations of H2 had no effect on the value of the ratio k(OH þ CF3CHO)/k(OH þ CH3CH3) lending support to the assumption that hydrogen acted as a scavenger for CF3O radicals. The OH reaction rate coefficient of CF3CH2CHO was measured relative to CH3CH2OH. Relative concentrations of both reactants were determined by analysing parts of the C–H stretching regions of CF3CH2CHO and CH3CH2OH (3100–2600 cm1). FTIR reference spectra of CF3CH2CHO, CH3CH2OH, CD3CH(ONO)CD3 , CF3CHO, CH3CHO, HCHO, NO2 and a sloping baseline were included in the spectral subtractions. In addition, we also included two weak spectra of yet unidentified compounds in the spectral subtractions. The first spectrum had a band at 2880 cm1 that came up together with the injection of CD3CH(ONO)CD3 into the reaction chamber, suggesting that the synthesised CD3CH(ONO)CD3 contained an impurity. The second spectrum had a band at 3031 cm1 and originated from a product as it grew in during the reaction. The two spectra were obtained in a separate experiment, that is, not in one of the experiments that Table 3 Some key reactions used in the FACSIMILE kinetic model of the CF3CHO/CH3CH3/O3/H2 reaction system. The complete set of reactions are given in Table S3y Fig. 3 FTIR spectra of the reaction mixture CF3CHO/CH3CH3/ H2/O3 : (A) before reaction with OH; (B) after reaction with OH; (C) residual after spectral subtraction analysis of spectrum A, see text for a list of reference spectra included in the subtraction; (D) residual after spectral subtraction analysis of spectrum B; (E) reference spectrum of CF3CHO; (F) reference spectrum of CH3CH3 . The spectra C–F are shifted for clarity. Reactions k298 K/1013 cm3 molecule1 s1 OH þ H2 ! H2O þ H OH þ CH3CH3 ! H2O þ CH2CH3 OH þ CF3CHO ! H2O þ CF3CO CF3O þ H2 ! CF3OH þ H CF3O þ CH3CH3 ! CF3OH þ CH2CH3 CF3O þ CF3CHO ! CF3OH þ CF3CO 0.067a 2.40b 4.80c 0.2d 12.3a 30.0d a Atkinson et al.23 b Sander et al.27 (see text for details). d This journal is Q The Owner Societies 2004 c This work. Estimated value Phys. Chem. Chem. Phys., 2004, 6, 1243–1252 1247 were used to determine the relative OH reaction rate coefficient of CF3CH2CHO. Fig. 5 shows an example of the course of reaction from one of the relative rate experiments together with the residuals after the spectral subtractions. A plot of the logarithm of the relative concentrations of CF3CH2CHO versus those of CH3CH2OH is shown in Fig. 6a. From the slope of the plot, a relative reaction rate coefficient of 1.21(5) was determined for the reaction between CF3CH2CHO and OH radicals. The latest JPL data evaluation27 gives the OH reaction rate coefficient for CH3CH2OH as 3.2 1012 cm3 molecule1 s1 and hence the derived absolute OH reaction rate coefficient for CF3CH2CHO is 3.87(16) 1012 cm3 molecule1 s1. In the ‘‘ Dublin experiments ’’, the OH reaction rate coefficient of CF3CH2CHO was measured relative to that for reaction with HC(O)OC2H5 . The experimental values of [A]0/[A]t and [R]0/[R]t determined by GC analysis have estimated errors of 2%. The concentration–time data were plotted according to eqn. (II) and gave a linear relationship with near-zero intercept, shown in Fig. 6b. From the slope of the plot, it was found that k(OH þ CF3CH2CHO)/k(OH þ HC(O)OC2H5) ¼ 3.51(9). The OH reaction rate coefficient of HC(O)OC2H5 has been measured by Wallington et al.30 (1.02(14) 1012 cm3 molecule1 s1) and Le Calve et al.31 (8.52(75) 1013 cm3 molecule1 s1). Using an average of these two values, 0.94 1012 cm3 molecule1 s1, an absolute rate coefficient of 3.30(8) 1012 cm3 molecule1 s1 is calculated for CF3CH2CHO. The errors quoted in the rate coefficients reported in this work are twice the standard deviation arising from the least-squares fit of the relative rate data and do not include an estimate of the error in the reference rate coefficient. 3.3. Effective quantum yield of photolysis Photolysis experiments with CF3CHO and CF3CH2CHO have been carried out at the EUPHORE simulation chamber in Valencia, Spain (longitude ¼ 0.5 , latitude ¼ 39.5 ) during the month of June. The solar actinic fluxes during the two experiments are shown in Fig. 7a and b in terms of the photolysis rate coefficient of NO2 , J(NO2), and the photolytic production rate coefficient of O(1D), J(O(1D)). The pressure and the temperature inside the chamber were not constant during the experiments. The observed losses of SF6 , DNBE, CF3CHO and CF3CH2CHO were therefore corrected Fig. 5 FTIR spectra of the reaction mixture CF3CH2CHO/ CH3CH2OH/CD3CH(ONO)CD3 : (A) before reaction with OH; (B) after reaction with OH; (C) residual after spectral subtraction analysis of spectrum A, see text for a list of reference spectra included in the subtraction; (D) residual after spectral subtraction analysis of spectrum B; (E) reference spectrum of CH3CH2OH; (F) reference spectrum of CF3CH2CHO. The residual spectra are magnified 10 times. The spectra C–F are shifted for clarity. 1248 Phys. Chem. Chem. Phys., 2004, 6, 1243–1252 Fig. 6 (a) Decay of CF3CH2CHO versus CH3CH2OH in the presence of OH radicals at 298(2) K as measured from three independent experiments. The uncertainty in each data point is based on an estimated uncertainty of 0.01 in the relative concentrations, while the uncertainty of the linear regression coefficients y ¼ 0.0071(23) þ 1.208(25) represents 1s. Two data points were excluded in the analysis, see text. (b) Decay of CF3CH2CHO versus HC(O)OC2H5 in the presence of OH radicals at 298(2) K: krel ¼ 3.51(9) 2s . according to the changes in pressure and temperature using the ideal gas law. From a least-squares analysis of the disappearance of SF6 (Fig. 8a), the leak rate coefficient during the CF3CHO photolysis experiment was found to be 7.51(32) 106 s1 (2s). At the same time the total removal rate coefficient of DNBE was determined to be 8.38(30) 105 s1. In Fig. 8b, the decay of CF3CHO is given as a plot of ln{[CF3CHO]0/[CF3CHO]t} versus the photolysis time. The total removal rate coefficient of CF3CHO was found to be 7.74(54) 106 s1 which is within experimental error of the leak rate. A least-squares analysis of the disappearance of CF3CHO according to eqn. (IV), i.e. correcting for loss of CF3CHO caused by leakage and reaction with OH radicals, give an upper limit for Jobs of 8.5 107 s1. The time averaged maximum photolysis rate coefficient, Jmax (see eqn. (VI)), during the experiment was calculated to be 5.5 105 s1. We therefore suggest that Feff < 2 102, which provides an upper limit for the effective quantum yield for the photolysis of CF3CHO. During the CF3CH2CHO experiment, the leak rate was found to be 5.18(62) 106 s1 as measured from the disappearance of SF6 (Fig. 9a). The observed total removal rates of DNBE and CF3CH2CHO were 2.72(30) 105 s1 and 7.52(29) 106 s1, respectively (Fig. 9b). After correcting for loss of CF3CH2CHO caused by leakage and reaction with OH radicals, the upper limit for Jobs is 1.5 106 s1. During This journal is Q The Owner Societies 2004 Fig. 7 Solar actinic fluxes during the photolysis experiments of CF3CHO (June 21, 2002) and CF3CH2CHO (June 26, 2002) at EUPHORE in terms of (a) the photolysis rate coefficient of NO2 , J(NO2), and (b) the photolytic production rate coefficient of O(1D), J(O(1D)). The steep increases in the actinic fluxes are due to opening of the reaction chamber. the experiment, Jmax was calculated to be 3.4 105 s1. This suggests that Feff < 4 102 for the photolysis of CF3CH2CHO. 4. Discussion 4.1. IR and UV-Vis absorption cross-sections As aforementioned, the only previous quantitative measurement of the infrared absorption intensities of CF3CHO was the study by Francisco and Williams.14 Over the wavenumber range 2890–801 cm1, Francisco and Williams reported that the integrated absorption intensity was 2.7(3) 1017 cm molecule1 for pure vapour and 10.7(6) 1017 cm molecule1 with argon added. This is significantly different from the measurement reported in this work. Over the wavenumber range 3000–775 cm1, we measured an integrated absorption intensity of 12.74(12) 1017 cm molecule1 for pure vapour. We offer no explanation to this discrepancy. We can only state that we checked for impurities and that we have tested our experimental setup against HCFC-22. The absorption intensities of HCFC-22 have been critically evaluated by Ballard et al.32 and are therefore well known. Our measurements of HCFC22 were within 5% of the absorption intensities reported by Ballard et al. We therefore believe that our measurements of Fig. 8 (a) Leakage as measured from the disappearance of SF6 during the photolysis experiment with CF3CHO in the EUPHORE simulation chamber. Leakage rate coefficient: kleak ¼ 7.51(16) 106 s1. (b) Decay of CF3CHO during exposure to pseudo-natural sunlight. Total removal rate coefficient: ktotal ¼ 7.74(27) 106 s1. The quoted uncertainty in the rate coefficients is 1s from the statistical analyses. The data points have been corrected for changes in temperature and pressure during the experiment. CF3CHO and CF3CH2CHO are not affected by any large systematic errors. As can be seen from Fig. 2a, the UV-Vis absorption crosssections of CF3CHO measured in this work are within the experimental uncertainties reported by Meller et al.16 and Francisco and Williams.14 The absorption cross-sections measured by Libuda15 seem to be too low. The UV-Vis spectra of CF3CHO and CF3CH2CHO (Fig. 2a and b) show a weak absorption below 220 nm. This is clearly different from CH3CHO and CH3CH2CHO.25 The corresponding acids have bands in this region.16 However, we have not seen any infrared absorption bands that could be attributed to either CF3COOH or CF3CH2COOH. Unfortunately, Meller et al.,16 Libuda15 and Francisco and Williams14 did not report absorption cross-sections in this wavelength region, but in Fig. 2 of the paper by Francisco and Williams,14 it can be seen that the absorbance for CF3CHO is non-zero below 220 nm. 4.2. OH-initiated oxidation We have measured a rate coefficient equal to 4.80(30) 1013 cm3 molecule1 s1 for the reaction between OH and CF3CHO, relative to CH3CH3 . This value is somewhat lower than the rate coefficients reported by Dóbé et al.,7 Scollard et al.8 and Laverdet et al.9 The OH reaction rate coefficient This journal is Q The Owner Societies 2004 Phys. Chem. Chem. Phys., 2004, 6, 1243–1252 1249 Fig. 9 (a) Leakage as measured from the disappearance of SF6 during the photolysis experiment with CF3CH2CHO in the EUPHORE simulation chamber. Leakage rate coefficient: kleak ¼ 5.18(31) 106 s1. (b) Decay of CF3CH2CHO during exposure of pseudo-natural sunlight. Total removal rate coefficient: ktotal ¼ 7.52(15) 106 s1. The quoted uncertainty in the rate coefficients is 1s from the statistical analyses. The data points have been corrected for changes in temperature and pressure during the experiment. for CH3CH3 is one of the best-known rate coefficients available in the literature, so it is unlikely that the discrepancy is due to the choice of CH3CH3 as reference compound. Scollard et al.8 reported that k(OH þ CF3CHO)/k(OH þ CH3C(O)CH3) ¼ 2.43(53) and k(Cl þ CF3CHO)/k(Cl þ CH3C(O)CH3) ¼ 1.14(4). In the latest JPL data evaluation,27 the recommended OH reaction rate coefficient for CH3C(O)CH3 is: k(T ) ¼ [1.33 1013 þ 3.82 1011exp(2000 K/T )] cm3 molecule1 s1. Using this expression, we have recalculated the rate coefficient from the relative rate measurements of Scollard et al.8 to be k(OH þ CF3CHO) ¼ 4.4(9) 1013 cm3 molecule1 s1 at 298 K. The work by Scollard et al. is now in quite excellent agreement with the present work. It appears that the three absolute rate coefficients7–9 determined for the reaction of OH with CF3CHO are all slightly higher than the relative rate measurements. This may be due to small amounts of reactive impurities in the CF3CHO used in the three studies. It is of interest to compare the OH reaction rate coefficient for reaction with CF3CHO with the OH rate coefficient for CF3CF2CHO recently determined by Sulbaek Andersen et al.33 Using an indirect relative rate technique, Sulbaek Andersen et al.33 measured a rate coefficient of 5.26(80) 1013 cm3 molecule1 s1 and as may be expected CF3CHO and CF3CF2CHO have similar reactivity towards the OH radical. 1250 Phys. Chem. Chem. Phys., 2004, 6, 1243–1252 Two different experimental setups have been used to measure the relative OH reaction rate coefficient of CF3CH2CHO. A rate coefficient of 3.87(16) 1012 cm3 molecule1 s1 was measured using CH3CH2OH as the reference compound (Oslo). As can be seen in Fig. 6a, there is a slight curvature on the logarithmic plot at the highest conversion of reactants. Because of this, two of the data points were excluded in the least-squares analysis. This curvature could be due to secondary reactions involving the CF3O radical since no scavenger was used. Even though CF3O will be produced only at a late stage in the reaction event,4 its reactivity towards CF3CH2CHO and CH3CH2OH may be larger than its reactivity towards the other compounds in the chamber. We do not believe however, that our results are seriously affected by this. When HC(O)OC2H5 was used as reference compound (Dublin), a rate coefficient of 3.30(8) 1012 cm3 molecule1 s1 was found. As can be seen, the difference between these two rate coefficients lie outside the quoted combined experimental errors. However, the quoted error limits reflect precision only and do not include errors in the reference rate constants, which probably add about a further 10% to the quoted errors. We prefer to quote a value of k(OH þ CF3CH2CHO) ¼ 3.6(3) 1012 cm3 molecule1 s1 for the rate coefficient. The major reaction pathway for reaction of OH radicals with aliphatic aldehydes is hydrogen atom abstraction from the aldehydic group.34 The rate coefficient for reaction of OH with CF3CHO is around a factor of 30 lower than for reaction with acetaldehyde.30 This result can be rationalized in terms of changes in the overall enthalpy of reaction and/ or destabilizing polar effects in the transition states for the reactions. The reported experimental values for the aldehydic C–H bond dissociation energies in CH3CHO and CF3CHO are 355 and 381 kJ mol1, respectively,35 and thus reaction with OH radicals are both strongly exothermic, D(H–OH) ¼ 4.91 kJ mol1.35 Rayez et al.12 have estimated that because of the difference in enthalpy changes for the two reactions, the rate coefficient for the reaction of OH radicals with CF3CHO will be lower than the value for the corresponding reaction with CH3CHO by a factor of less than 2.5 at 298 K. They attributed the significant reduction in the reactivity of CF3CHO compared to CH3CHO to destabilization of the transition state for reaction of OH with CF3CHO by the electron withdrawing inductive effect of the–CF3 group. The rate coefficient for the reaction of OH with CF3CH2CHO is about five times smaller than for reaction with CH3CH2CHO.34 Since the aldehydic C–H bond strengths in these two molecules would be expected to be quite similar,35 the reduction in reactivity of the b-substituted fluorinated aldehyde must reflect the long range destabilizing inductive effect of the –CF3 group in the transition state. Kwok and Atkinson36 have previously found that rate coefficients estimated from simple structure–activity relationships (SAR), which consider only next-neighbour atomic groups, result in higher values than experimentally observed when applied to reactions of OH with fluorinated compounds. They pointed out that the long range deactivating effect of fluorinated groups must be incorporated into the relationships to obtain reasonable agreement between calculated and experimental rate data. 4.3. Photolysis Under pseudo-natural conditions in the EUPHORE simulation chamber, it has been found that the effective quantum yield of photolysis for CF3CHO and CF3CH2CHO are <2 102 and <4 102, respectively. For CF3CHO, this is in contrast to the quantum yields reported by Dodd and Smith,17 who observed a quantum yield of 0.12 for the radical channel yielding CF3 and HCO following photolysis at 313 nm and 40–53 hPa at room temperature. A possible explanation This journal is Q The Owner Societies 2004 for this discrepancy is that the intensity of the sunlight is quite low at wavelengths below 320 nm. Further, the photodissociation quantum yield has been shown to be strongly pressure dependent, decreasing with increasing pressure.18 The effective quantum yields are considerably lower than those found for CH3CHO and CH3CH2CHO. In the EU project ‘‘ RADICAL ’’,37 it was found that the effective quantum yields of CH3CHO and CH3CH2CHO were 0.06 0.1 and 0.25 0.04, respectively, determined during weather conditions similar to those during this work. Yadav and Goddard38 and Francisco39 have studied the dissociation reactions of CH3CHO and CF3CHO, respectively, by ab initio calculations of quite similar levels. The results indicate that the barriers towards dissociation do not change much upon fluorination. However, both calculations were carried out using rather small basis sets without including diffuse functions which are important when describing loosely bound electrons.40 Further, the geometries were only optimised at the Hartree–Fock level of theory. An interesting question is what effect fluorine substitution in the CH3 groups of CH3CHO and CH3CH2CHO has on the relative importance of internal conversion (S1 ! S0) or intersystem crossing (S1 ! T1), compared to the efficiency of relaxation of the S1 state by fluorescence. In laser-induced fluorescence experiments with CF3CHO, fluorescence has been observed up to 37 000 cm1 (270 nm).41 In contrast, the fluorescence excitation spectrum of CH3CHO has very low intensity above 31 700 cm1 (315 nm).42 According to Robb and co-workers,43,44 emission from excited states implies that there is no accessible surface crossing promoting fast radiation-less decay: the existence or lack of a crossing depends on the electronic structure of the two states and is not a simple function of the energy gap. However, the very low effective quantum yield of CF3CH2CHO compared to CH3CH2CHO is surprising. We are therefore currently investigating these issues further. 4.4. Atmospheric lifetimes and global warming potentials The atmospheric lifetimes, t, of CF3CHO and CF3CH2CHO due to removal by reaction with OH radicals and photolysis may be estimated from the data obtained in this study. The atmospheric lifetime is given by t1 ¼ tOH1 þ tphotol1.45 Using the determined OH rate coefficients, a global averaged concentration of OH radicals equal to 9.4 105 radicals cm3 (ref. 46) and the photolysis rates measured in this work, the following lifetimes of CF3CHO and CF3CH2CHO in the gas-phase are found: tOH(CF3CHO) 26 days; tphotol(CF3CHO) > 27 days; tOH(CF3CH2CHO) 4 days; tphotol(CF3CH2CHO) > 15 days (the photolytic lifetimes are lower limits and the true photolytic lifetimes are likely to be longer). The results suggest that reaction with OH or photolysis may both be important sinks for CF3CHO. Fluorinated aldehydes are fairly soluble in water and undergo hydrolysis and oxidation forming the corresponding carboxylic acids. Since the lifetimes of CF3CHO with respect to loss by reaction with OH or photolysis are relatively long, uptake in rain water or cloud droplets may be an important sink for CF3CHO. The tropospheric lifetime of soluble species is of the order of 20 days and hence CF3CHO could provide a source of CF3COOH in the atmosphere. The major fate of CF3CH2CHO in the troposphere would appear to be reaction with OH although photolysis may also be of some importance. The available data suggest that the primary product of both these sinks is CF3CHO4 and hence the atmospheric degradation of CF3CH2CHO may provide an additional source of CF3COOH in the environment. Pinnock et al.47 have provided a simple method for estimating the instantaneous cloudy-sky radiative forcing (IF) directly from a molecule’s absorption cross-sections. Global Table 4 Estimated global warming potentials, GWP(t), of CF3CHO and CF3CH2CHO for a 20 year time horizon, relative to CFC-11. The instantaneous cloudy-sky radiative forcings (IF) for a 1 ppbv increase in atmospheric concentrations was calculated according to the procedure given by Pinnock et al.47 The data on CFC-11 were taken from the paper by Pinnock et al. See text for details on the calculation of the atmospheric lifetimes, t, of CF3CHO and CF3CH2CHO Compound CF3CHO CF3CH2CHO CFC-11 Wavenumber region/cm1 IF/ W m2 t/ year GWP(20) 1450–465 1475–505 0.129 0.132 0.26 0.36 0.008 50.0 0.0015 0.0003 1.0000 warming potentials, GWP(t), for CF3CHO and CF3CH2CHO, relative to CFC-11, can then be calculated from the following expression:48 GWPðtÞ ¼ IFald tald Mald IFCFC11 tCFC11 MCFC11 1 expðt=tald Þ ; 1 expðt=tCFC11 Þ ð7Þ where M is the molecular mass and t is the time horizon over which the instantaneous forcing is integrated. Instantaneous forcings and global warming potentials for a 20-year time horizon for CF3CHO and CF3CH2CHO are collected in Table 4. The data on CFC-11 were taken from the work of Pinnock et al.47 Although the instantaneous forcings of CF3CHO and CF3CH2CHO are relatively large compared to that of CFC-11, their global warming potentials are negligible due to the short lifetimes. Care must be exercised when applying these results. In order to provide realistic predictions, advanced three-dimensional chemical tracer modelling and radiative forcing calculations are needed. However, we justify the calculations because they provide a reasonable estimate of the atmospheric lifetimes and global warming potentials of CF3CHO and CF3CH2CHO. This information is important when assessing the total environmental burden of possible HCFC/HFC replacement compounds. Acknowledgements This work is part of the project ‘‘ Impact of Fluorinated Alcohols and Ethers on the Environment ’’, and has received support from the Commission of the European Communities under the Energy, Environment and Sustainable Development Programme through contract EVK2-CT-1999-00009. We thank Klaus Wirtz and his team for all their help during the stay at EUPHORE. SRS acknowledges F. Temps for helpful discussions concerning the photolysis of CF3CHO. References 1 T. J. Wallington, P. Dagaut and M. J. Kurylo, J. Phys. Chem., 1988, 92, 5024–5028. 2 K. Tokuhashi, H. Nagai, A. Takahashi, M. Kaise, S. Kondo, A. Sekiya, M. Takahashi, Y. Gotoh and A. Suga, J. Phys. Chem. A, 1999, 103, 2664–2672. 3 V. C. Papadimitriou, A. V. Prosmitis, Y. G. Lazarou and P. Papagiannakopoulos, J. Phys. Chem. A, 2003, 107, 3733–3740. 4 I. Magneron, V. Bossontrot, A. Mellouki, G. LeBras, T. Kelly, J. Treacy and H. Sidebottom, Kinetics and mechanisms for the oxidation of fluoroalcohols under atmospheric conditions, manuscript in preparation. This journal is Q The Owner Societies 2004 Phys. Chem. Chem. Phys., 2004, 6, 1243–1252 1251 5 S. R. Sellevåg, C. J. Nielsen, O. A. Søvde, G. Myhre, J. K. Sundet, F. Stordal and I. S. A. Isaksen, Atmos. Environ., 2004, submitted. 6 T. J. Wallington, W. F. Schneider, O. J. Nielsen, J. Sehested, D. R. Worsnop, W. J. De Bruyn and J. A. Shorter, in Halon Replacements: Technology and Science, ed. A. W. Miziolek and W. Tsang, American Chemical Society, Washington DC, 1995, pp. 16–30. 7 S. Dóbé, L. A. Khachatryan and T. Berces, Ber. Bunsen-Ges. Phys. Chem., 1989, 93, 847–852. 8 D. J. Scollard, J. J. Treacy, H. W. Sidebottom, C. BalestraGarcia, G. Laverdet, G. LeBras, H. MacLeod and S. Teton, J. Phys. Chem., 1993, 97, 4683–4688. 9 G. Laverdet, G. LeBras, H. MacLeod, G. Poulet, S. Teton, D. J. Scollard, J. J. Treacy and H. W. Sidebottom, Proc. SPIE-Int. Soc. Opt. Eng., 1993, 1715, 100–112. 10 J. S. Francisco, J. Chem. Soc., Faraday Trans., 1992, 88, 1943–1947. 11 M. T. Rayez, J. C. Rayez, T. Berces and G. Lendvay, J. Phys. Chem., 1993, 97, 5570–5576. 12 M. T. Rayez, D. J. Scollard, H. W. Sidebottom, C. BalestraGarcia, S. Teton and G. Le Bras, Chem. Phys. Lett., 1994, 223, 452–458. 13 A. K. Chandra, T. Uchimaru and M. Sugie, Phys. Chem. Chem. Phys., 2001, 3, 3961–3966. 14 J. S. Francisco and I. H. Williams, Mol. Phys., 1992, 76, 1433–1441. 15 H.-G. Libuda, PhD Thesis, Bergischen Universität-Gesamthochschule, Wuppertal, 1992. 16 R. Meller, D. Boglu and G. K. Moortgat, STEP-HALOCSIDE/ AFEAS Workshop, Dublin, 23–25 March, 1993, pp. 130–138. 17 R. E. Dodd and J. W. Smith, J. Chem. Soc., 1957, 1465–1473. 18 C. Pearce and D. A. Whytock, J. Chem. Soc., Chem. Commun., 1971, 1464–1466. 19 H. R. Richer, J. R. Sodeau and I. Barnes, STEP-HALOCSIDE/ AFEAS Workshop, Dublin, 23–25 March, 1993, pp. 182–188. 20 T. J. Wallington and O. J. Nielsen, in General Aspects of the Chemistry of Radicals, ed. Z. B. Alfassi, John Wiley & Sons, Chichester, 1999, pp. 19–50. 21 K. H. Becker, The European Photoreactor EUPHORE. Design and Technical Development of the European Photoreactor and First Experimental Results, Final Report of the EC-Project Contract EV5V-CT92-0059, Wuppertal, Germany, 1996. 22 F. Kramp and S. E. Paulson, J. Phys. Chem. A, 1998, 102, 2685–2690. 23 R. Atkinson, D. L. Baulch, R. A. Cox, R. F. Hampson, Jr., J. A. Kerr, M. J. Rossi and J. Troe, J. Phys. Chem. Ref. Data, 1997, 26, 521–1013. 24 W. A. Noyes, Org. Synth., 1943, Collect. Vol. 2, 108–109. 25 R. D. Martinez, A. A. Buitrago, N. W. Howell, C. H. Hearn and J. A. Joens, Atmos. Environ., Part A, 1992, 26, 785–792. 26 D. York, Can. J. Phys., 1966, 44, 1079–1086. 27 S. P. Sander, R. R. Friedl, D. M. Golden, M. J. Kurylo, R. E. Huie, V. L. Orkin, G. K. Moortgat, A. R. Ravishankara, C. E. Kolb, M. J. Molina and B. J. Finlayson-Pitts, Chemical Kinetics and Photochemical Data for Use in Atmospheric Studies. 1252 Phys. Chem. Chem. Phys., 2004, 6, 1243–1252 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 Evaluation Number 14, National Aeronautics and Space Administration, Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, 2003. FACSIMILE Version 3.0.30, AEA Technology plc, 1998. NIST Chemical Kinetics Database, NIST Standard Reference Database 17-2Q98, National Institute of Standards and Technology, Gaithersburg, MD 20 899 USA. T. J. Wallington, P. Dagaut, R. Liu and M. J. Kurylo, Int. J. Chem. Kinet., 1988, 20, 177–186. S. Le Calve, G. Le Bras and A. Mellouki, J. Phys. Chem. A, 1997, 101, 5489–5493. J. Ballard, R. J. Knight, D. A. Newnham, J. Vander Auwera, M. Herman, G. Di Lonardo, G. Masciarelli, F. M. Nicolaisen, J. A. Beukes, L. K. Christensen, R. McPheat, G. Duxbury, R. Freckleton and K. P. Shine, J. Quant. Spectrosc. Radiat. Transfer, 2000, 66, 109–128. M. P. Sulbaek Andersen, M. D. Hurley, T. J. Wallington, J. C. Ball, J. W. Martin, D. A. Ellis, S. A. Mabury and O. J. Nielsen, Chem. Phys. Lett., 2003, 379, 28–36. R. Atkinson, J. Phys. Chem. Ref. Data, Monogr., 1994, 2, 1–216. D. F. McMillen and D. M. Golden, Annu. Rev. Phys. Chem., 1982, 33, 493–532. E. S. C. Kwok and R. Atkinson, Atmos. Environ., 1995, 29, 1685–1695. G. K. Moortgat, Evaluation of Radical Sources in Atmospheric Chemistry through Chamber and Laboratory Studies: RADICAL, Final report on EU project ENV4-CT97-0419, MaxPlanck-Institut für Chemie, Atmospheric Chemistry Division, Mainz, Germany, 2000. J. S. Yadav and J. D. Goddard, J. Chem. Phys., 1986, 84, 2682–2690. J. S. Francisco, Chem. Phys., 1992, 163, 27–36. T. Helgaker, P. Jørgensen and J. Olsen, Molecular ElectronicStructure Theory, John Wiley & Sons Ltd, Chichester, 2000. F. Temps, private communication. G.-H. Leu, C.-L. Huang, S.-H. Lee, Y.-C. Lee and I. C. Chen, J. Chem. Phys., 1998, 109, 9340–9350. F. Bernardi, M. Olivucci and M. A. Robb, Chem. Soc. Rev., 1996, 25, 321–328. M. J. Bearpark and M. A. Robb, J. Phys. Chem. A, 2000, 104, 1075–1077. R. P. Wayne, Chemistry of Atmospheres, Oxford University Press, Oxford, UK, 3rd edn., 2000. R. G. Prinn, J. Huang, R. F. Weiss, D. M. Cunnold, P. J. Fraser, P. G. Simmonds, A. McCulloch, C. Harth, P. Salameh, S. O’Doherty, R. H. J. Wang, L. Porter and B. R. Miller, Science, 2001, 292, 1882–1887. S. Pinnock, M. D. Hurley, K. P. Shine, T. J. Wallington and T. J. Smyth, J. Geophys. Res. [Atmos.], 1995, 100, 23 227–23 238. Climate Change 1994: Radiative Forcing of Climate Change and An Evaluation of the IPCC IS92 Emission Scenarios, ed. J. T. Houghton, L. G. Meira Filho, J. Bruce, H. Lee, B. A. Callander, E. Haites, N. Harris and K. Maskell, Intergovernmental Panel on Climate Change, Cambridge University Press, Cambridge, 1995. This journal is Q The Owner Societies 2004
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