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Atmospheric reaction of methyl mercaptan with hydroxyl radical as an acid rain primary agent.

ABSTRACT: For the CH₃SH?+?OH atmospheric reaction, we study the mechanism, potential energy surface, thermodynamic parameters of all stationary points, and rate of generation of the main product channels at high, low, and intermediate pressures. In this study, the UMP2, UM062X, UB3LYP, and CCSD(T) methods by Dunning and Pople basis sets are used and the results are compared with the experimental data. It is theoretically predicted that the reaction has fourteen possible pathways with eight different products in the gas phase. The thermodynamic results show that OH radical extracts predominantly the hydrogen of the SH functional group compared to the hydrogen of the CH₃ group of CH₃SH. Also, the rate constant calculations indicate that the extraction of the hydrogen atom of the SH group has a major role in 150-3000 K, while a good contribution is observed for the hydrogen of methyl group above 1200 K. Our results show that the used methods lead to good agreement with experiment. Finally, we demonstrated that why the main path is the main path.

SUBMITTER: Douroudgari H

PROVIDER: S-EPMC7583294 | biostudies-literature | 2020 Oct

REPOSITORIES: biostudies-literature

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Atmospheric reaction of methyl mercaptan with hydroxyl radical as an acid rain primary agent.

Douroudgari Hamed H Vahedpour Morteza M Mohammadi Samane S

Scientific reports 20201022 1

For the CH<sub>3</sub>SH + OH atmospheric reaction, we study the mechanism, potential energy surface, thermodynamic parameters of all stationary points, and rate of generation of the main product channels at high, low, and intermediate pressures. In this study, the UMP2, UM062X, UB3LYP, and CCSD(T) methods by Dunning and Pople basis sets are used and the results are compared with the experimental data. It is theoretically predicted that the reaction has fourteen possible pathways with eight diff ...[more]

PMID: 33093495

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Project description:Understanding the mechanism of hydrazine oxidation reaction by OH radical along with the rate constants of all possible pathways leads to explain the fate of hydrazine in the atmosphere. In this article, the comprehensive mechanisms and kinetics of the hydrazine plus hydroxyl radical reaction have been investigated theoretically at different temperatures and pressures. To achieve the main goals, a series of high levels of quantum chemical calculations have been widely implemented in reliable channels of the H-abstraction, SN2, and addition/elimination reactions. The energy profile of all pathways accompanied by the molecular properties of the involved stationary points has been characterized at the MP2, M06-2X, and CCSD(T)/CBS levels. To estimate accurate barrier energies of the H-abstraction channels, large numbers of the CCSD (T) calculations in conjunction with various augmented basis sets have been implemented. The direct dynamic calculations have been carried out using the validated M06-2X/maug-cc-pVTZ level, and also by the CCSD(T) (energies) + MP2 (partition functions) level. The pressure-dependent rate constants of the barrierless pathways have been investigated by the strong collision approach. Therefore, the main behaviors of the N2H4 + OH reaction have been explored according to the influences of temperature and pressure on the computed rate coefficients within the well-behaved theoretical frameworks of the TST, VTST, and RRKM theories. It has been found that the H-abstraction mechanism (to form N2H3) is dominant relative to the SN2 reaction and OH-addition to the N center of N2H4 moiety (to form H2NOH + NH2). The computed high pressure limit rate constant of the main reaction pathway, k(298.15) = 7.31 × 10-11 cm3 molecule-1 s-1, has an excellent agreement with the experimental value (k (298.15) = (6.50 ± 1.3) × 10-11 cm3 molecule-1 s-1) recommended by Vaghjiani. Also, the atmospheric lifetime of hydrazine degradation by OH radicals has been demonstrated to be 32.80 to 1161.11 h at the altitudes of 0-50 km. Finally, the disagreement in the calculated rate constants between the previous theoretical study and experimental results has been rectified.

Dataset Information

Atmospheric reaction of methyl mercaptan with hydroxyl radical as an acid rain primary agent.

Publications

Atmospheric reaction of methyl mercaptan with hydroxyl radical as an acid rain primary agent.

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