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dc.contributor.authorStraccia Cepeda, Vianni-
dc.contributor.authorCardona, Alejandro L.-
dc.contributor.authorBlanco, María Belén-
dc.contributor.authorVentura, Oscar N.-
dc.contributor.authorTeruel, Mariano A.-
dc.date.accessioned2025-05-09T17:29:27Z-
dc.date.available2025-05-09T17:29:27Z-
dc.date.issued2024-
dc.identifier.citationStraccia Cepeda, V., Cardona, A., Blanco, M. y otros. "Theoretical and in-situ FTIR study of the atmospheric sink of methyl dichloroacetate (MDCA) by •OH radicals and Cl• atoms : Kinetics, product distribution and mechanism". [en línea] ACS Earth and Space Chemistry [en línea] v.8, nº 12, 2024. 34 p. DOI: 10.1021/acsearthspacechem.4c00264es
dc.identifier.urihttps://hdl.handle.net/20.500.12008/49965-
dc.descriptionPostprint. La versión final fue publicada en: https://pubs.acs.org/doi/10.1021/acsearthspacechem.4c00264es
dc.description.abstractThe 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.es
dc.description.sponsorshipAlexander von Humboldt Foundationes
dc.description.sponsorshipAgencia Nacional de Investigación e Innovación (Uruguay)es
dc.description.sponsorshipConsejo Superior de Investigaciones Científicas (Uruguay)es
dc.description.sponsorshipConsejo Nacional de Investigaciones Científicas y Técnicas (Argentina)es
dc.format.extent34 p.es
dc.format.mimetypeapplication/pdfes
dc.language.isoenes
dc.publisherAmerican Chemical Societyes
dc.relation.isformatofPDFes
dc.relation.ispartofACS Earth and Space Chemistry, v.8, nº 12, 2024es
dc.rightsLas obras depositadas en el Repositorio se rigen por la Ordenanza de los Derechos de la Propiedad Intelectual de la Universidad de la República.(Res. Nº 91 de C.D.C. de 8/III/1994 – D.O. 7/IV/1994) y por la Ordenanza del Repositorio Abierto de la Universidad de la República (Res. Nº 16 de C.D.C. de 07/10/2014)es
dc.subjectMethyl dichloroacetatees
dc.subjectFourier transform infraredes
dc.subjectPotential-Energy Surfacees
dc.subjectVolatile Organic Compoundses
dc.subjectAtmospheric oxidantses
dc.subjectDicloroacetato de metiloes
dc.subjectInfrarroja por Transformada de Fourieres
dc.subjectSuperficie de energía potenciales
dc.subjectCompuestos orgánicos volátileses
dc.subjectOxidantes atmosféricoses
dc.titleTheoretical and in-situ FTIR study of the atmospheric sink of methyl dichloroacetate (MDCA) by OH radicals and Cl atoms : Kinetics, product distribution and mechanismes
dc.typeArtículoes
dc.contributor.filiacionStraccia Cepeda Vianni, INFIQC (Argentina). Fisicoquímica-
dc.contributor.filiacionCardona Alejandro L., Universidad de la República (Uruguay). Facultad de Química. CCBG-DETEMA-
dc.contributor.filiacionBlanco María Belén, Universidad Nacional de Córdoba (Argentina). Facultad de Ciencias Exactas Físicas y Naturales. Laboratorio Universitario de Química y Contaminación del Aire (L.U.Q.C.A.). Instituto de Investigaciones en Fisicoquímica de Córdoba (I.N.F.I.Q.C.) ; CONICET. Departamento de Fisicoquímica. Facultad de Ciencias Químicas.-
dc.contributor.filiacionVentura Oscar N., Universidad de la República (Uruguay). CCBG-DETEMA-
dc.contributor.filiacionTeruel Mariano A., Universidad Nacional de Córdoba (Argentina). Facultad de Ciencias Exactas Físicas y Naturales. Laboratorio Universitario de Química y Contaminación del Aire (L.U.Q.C.A.). Instituto de Investigaciones en Fisicoquímica de Córdoba (I.N.F.I.Q.C.) ; CONICET. Departamento de Fisicoquímica. Facultad de Ciencias Químicas.-
dc.rights.licenceLicencia Creative Commons Atribución - No Comercial - Sin Derivadas (CC - By-NC-ND 4.0)es
dc.identifier.doi10.1021/acsearthspacechem.4c00264-
Aparece en las colecciones: Publicaciones académicas y científicas - Facultad de Química

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