FTIR gas-phase kinetic study on the reactions of some acrylate esters with OH radicals and Cl atoms

被引:2
作者
Moreno, A. [2 ]
Gallego-Iniesta, M. P. [1 ]
Taccone, R. [3 ]
Martin, M. P. [1 ]
Cabanas, B. [1 ]
Salgado, M. S. [1 ]
机构
[1] Univ Castilla La Mancha, Fac Ciencias Quim, Dept Quim Fis, E-13071 Ciudad Real, Spain
[2] Univ Castilla La Mancha, CYTEMA, ICCA, Inst Invest Combust & Contaminac Atmosfer, E-13071 Ciudad Real, Spain
[3] Univ Nacl Cordoba, Fac Ciencias Quim, Dept Fisicoquim, RA-5000 Cordoba, Argentina
关键词
Atmospheric chemistry; OH radical; Cl atoms; Rate coefficients; Acrylate esters; Relative technique; FTIR spectroscopy; VOLATILE ORGANIC-COMPOUNDS; RATE CONSTANTS; INITIATED DEGRADATION; METHYL ACRYLATE; ATMOSPHERIC HYDROXYL; UNSATURATED ESTERS; BOUNDARY-LAYER; BUTYL ACRYLATE; NO3; RADICALS; OZONE;
D O I
10.1007/s11356-014-3112-4
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Acrylate esters are alpha,beta-unsaturated esters that contain vinyl groups directly attached to the carbonyl carbon. These compounds are widely used in the production of plastics and resins. Atmospheric degradation processes of these compounds are currently not well understood. The kinetics of the gas phase reactions of OH radicals with methyl 3-methylacrylate and methyl 3,3-dimethylacrylate were determined using the relative rate technique in a 50 L Pyrex photoreactor using in situ FTIR spectroscopy at room temperature (298 +/- 2 K) and atmospheric pressure (708 +/- 8 Torr) with air as the bath gas. Rate coefficients obtained were (in units cm(3) molecule(-1) s(-1)): (3.27 +/- 0.33) x 10(-11) and (4.43 +/- 0.42) x 10(-11), for CH(3)CHa=CHC(O)OCH3 and (CH3)(2)CH=CHC(O)OCH3, respectively. The same technique was used to study the gas phase reactions of hexyl acrylate and ethyl hexyl acrylate with OH radicals and Cl atoms. In the experiments with Cl, N-2 and air were used as the bath gases. The following rate coefficients were obtained (in cm(3) molecule(-1) s(-1)): k(3) (CH2=CHC(O)O( CH2)(5)CH3 + Cl) = (3.31 +/- 0.31) x 10(-10), k(4)(CH2=CHC(O)OCH2CH(CH2CH3)(CH2)(3)CH3 + Cl) = (3.46 +/- 0.31) x 10(-10), k(5)(CH2=CHC(O)O(CH2)(5)CH3 + OH) = (2.28 +/- 0.23) x 10(-11), and k(6)(CH2=CHC(O)OCH2CH(CH2CH3)(CH2)(3)CH3 + OH) = (2.74 +/- 0.26) x 10(-11). The reactivity increased with the number of methyl substituents on the double bond and with the chain length of the alkyl group in -C(O)OR. Estimations of the atmospheric lifetimes clearly indicate that the dominant atmospheric loss process for these compounds is their daytime reaction with the hydroxyl radical. In coastal areas and in some polluted environments, Cl atom-initiated degradation of these compounds can be significant, if not dominant. Maximum Incremental Reactivity (MIR) index and global warming potential (GWP) were also calculated, and it was concluded that these compounds have significant MIR values, but they do not influence global warming.
引用
收藏
页码:11541 / 11551
页数:11
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