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Artículo

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

Straccia Cepeda, Vianni GiovannaIcon ; Ladino Cardona, Miyer AlejandroIcon ; Blanco, Maria BelenIcon ; Ventura, Oscar N.; Teruel, Mariano AndresIcon
Fecha de publicación: 12/2024
Editorial: American Chemical Society
Revista: ACS Earth and Space Chemistry
ISSN: 2472-3452
Idioma: Inglés
Tipo de recurso: Artículo publicado
Clasificación temática:
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Resumen

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.
Palabras clave: COMPUTACTIONAL , KINETIC , SUPERFICIE , VIBRATION
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info:eu-repo/semantics/restrictedAccess Excepto donde se diga explícitamente, este item se publica bajo la siguiente descripción: Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Unported (CC BY-NC-SA 2.5)
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URI: http://hdl.handle.net/11336/266255
URL: https://pubs.acs.org/doi/10.1021/acsearthspacechem.4c00264#
DOI: https://doi.org/10.1021/acsearthspacechem.4c00264
Colecciones
Articulos(INFIQC)
Articulos de INST.DE INVESTIGACIONES EN FISICO- QUIMICA DE CORDOBA
Citación
Straccia Cepeda, Vianni Giovanna; Ladino Cardona, Miyer Alejandro; Blanco, Maria Belen; Ventura, Oscar N.; Teruel, Mariano Andres; Theoretical and In Situ FTIR Studies of the Atmospheric Sink of Methyl Dichloroacetate by •OH Radicals and Cl• Atoms: Kinetics, Product Distribution, and Mechanism; American Chemical Society; ACS Earth and Space Chemistry; 8; 12; 12-2024; 2599-2610
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