Theoretical and In Situ FTIR Studies of the Atmospheric Sink of Methyl Dichloroacetate by <sup>•</sup>OH Radicals and Cl<sup>•</sup> Atoms: Kinetics, Product Distribution, and Mechanism

The atmospheric degradation of methyl dichloroacetate can be initiated by •OH and Cl• radicals through H atom abstraction from the alkyl groups (Cl2HC– or –CH3) of the chloroester. Product yields for the gas-phase reaction with •OH were determined experimentally in a 480 L Pyrex glass atmospheric-simulation reactor coupled to an in situ Fourier transform infrared (FTIR) spectrometer. In addition to those results, we present in this paper a complete degradation mechanism based on thermodynamic data obtained by identifying all critical points on the potential-energy surface for these reactions, employing density functional calculations with the M06-2X and MN15 hybrid exchange–correlation functionals and the aug-cc-pVTZ basis sets. A conformational search for reactants and transition states was performed. The energies of these conformers were later corrected at the CCSD(T,Full)-F12/complete basis set level by using the SVECV-f12 composite method. The corrected energies were then used to obtain the theoretical rate coefficients in a multiconformer approach. The global rate coefficient calculated for the reaction of methyl dichloroacetate with •Cl atoms is (7.34 × 10–12 cm3 molecule–1·s–1), and the global rate coefficient calculated for the reaction with •OH radicals is (1.07 × 10–12 cm3 molecule–1·s–1). The identified products and their respective yield percentages for the reaction of MDCA with •OH were Cl2CHCOOH (44 ± 3%), COCl2 (43 ± 3%), and CO (41 ± 6%). The analysis of the mechanism suggests that formation of P1 (Cl2CO, phosgene) occurs mainly by abstraction from the Cl2HC– group since the formation of P4 (Cl2CHC(O)OH, dichloroacetic acid) and P5 (CO, carbon monoxide) is more favorable in the path for abstraction from the –OCH3 group. The multiconformer calculated rate constant values were compared with the values obtained employing only the low-lying TSs and with our own previous experimental studies. Branching ratios for the reaction with •Cl were compared to the experimental product yields.

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Journal
ACS Earth and Space Chemistry
Published
2024-12-04
DOI
https://doi.org/10.1021/acsearthspacechem.4c00264
Citations
1
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
0.38

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article

Theoretical and In Situ FTIR Studies of the Atmospheric Sink of Methyl Dichloroacetate by •OH Radicals and Cl• Atoms: Kinetics, Product Distribution, and Mechanism

Marı́a B. Blanco, Oscar N. Ventura, Alejandro L. Cardona, Mariano A. Teruel et al.
1 citations
ACS Earth and Space Chemistry
Atmospheric chemistry and aerosols
0.38
article

Theoretical and In Situ FTIR Studies of the Atmospheric Sink of Methyl Dichloroacetate by •OH Radicals and Cl• Atoms: Kinetics, Product Distribution, and Mechanism

Marı́a B. Blanco, Oscar N. Ventura, Alejandro L. Cardona, Mariano A. Teruel, Vianni G. Straccia C
article en
1 citations

Abstract

The atmospheric degradation of methyl dichloroacetate can be initiated by •OH and Cl• radicals through H atom abstraction from the alkyl groups (Cl2HC– or –CH3) of the chloroester. Product yields for the gas-phase reaction with •OH were determined experimentally in a 480 L Pyrex glass atmospheric-simulation reactor coupled to an in situ Fourier transform infrared (FTIR) spectrometer. In addition to those results, we present in this paper a complete degradation mechanism based on thermodynamic data obtained by identifying all critical points on the potential-energy surface for these reactions, employing density functional calculations with the M06-2X and MN15 hybrid exchange–correlation functionals and the aug-cc-pVTZ basis sets. A conformational search for reactants and transition states was performed. The energies of these conformers were later corrected at the CCSD(T,Full)-F12/complete basis set level by using the SVECV-f12 composite method. The corrected energies were then used to obtain the theoretical rate coefficients in a multiconformer approach. The global rate coefficient calculated for the reaction of methyl dichloroacetate with •Cl atoms is (7.34 × 10–12 cm3 molecule–1·s–1), and the global rate coefficient calculated for the reaction with •OH radicals is (1.07 × 10–12 cm3 molecule–1·s–1). The identified products and their respective yield percentages for the reaction of MDCA with •OH were Cl2CHCOOH (44 ± 3%), COCl2 (43 ± 3%), and CO (41 ± 6%). The analysis of the mechanism suggests that formation of P1 (Cl2CO, phosgene) occurs mainly by abstraction from the Cl2HC– group since the formation of P4 (Cl2CHC(O)OH, dichloroacetic acid) and P5 (CO, carbon monoxide) is more favorable in the path for abstraction from the –OCH3 group. The multiconformer calculated rate constant values were compared with the values obtained employing only the low-lying TSs and with our own previous experimental studies. Branching ratios for the reaction with •Cl were compared to the experimental product yields.

ACS Earth and Space ChemistryVol. 8(12)
Consejo Nacional de Investigaciones Científicas y Técnicas (AR), Universidad Nacional de Córdoba (AR), University of Wuppertal (DE), Research Centre in Biological Chemistry of Córdoba (AR)
Alexander von Humboldt-Stiftung, Agencia Nacional de Investigación e Innovación, Consejo Nacional de Investigaciones Científicas y Técnicas, Secretaria de Ciencia y Tecnología - Universidad Nacional de Córdoba, Comisión Sectorial de Investigación Científica, Fondo para la Investigación Científica y Tecnológica
Openalex Percentile: Top 38%
Atmospheric chemistry and aerosols
0.38
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