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Rate Coefficients of the Reactions of Fluorine Atoms with H(2)S and SH over the Temperature Range 220–960 K

Reaction F + H(2)S→SH + HF (1) is an effective source of SH radicals and an important intermediate in atmospheric and combustion chemistry. We employed a discharge-flow, modulated molecular beam mass spectrometry technique to determine the rate coefficient of this reaction and that of the secondary...

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Detalles Bibliográficos
Autor principal: Bedjanian, Yuri
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9739569/
https://www.ncbi.nlm.nih.gov/pubmed/36500456
http://dx.doi.org/10.3390/molecules27238365
Descripción
Sumario:Reaction F + H(2)S→SH + HF (1) is an effective source of SH radicals and an important intermediate in atmospheric and combustion chemistry. We employed a discharge-flow, modulated molecular beam mass spectrometry technique to determine the rate coefficient of this reaction and that of the secondary one, F + SH→S + HF (2), at a total pressure of 2 Torr and in a wide temperature range 220–960 K. The rate coefficient of Reaction (1) was determined directly by monitoring consumption of F atoms under pseudo-first-order conditions in an excess of H(2)S. The rate coefficient of Reaction (2) was determined via monitoring the maximum concentration of the product of Reaction (1), SH radical, as a function of [H(2)S]. Both rate coefficients were found to be virtually independent of temperature in the entire temperature range of the study: k(1) = (1.86 ± 0.28) × 10(−10) and k(2) = (2.0 ± 0.40) × 10(−10) cm(3) molecule(−1) s(−1). The kinetic data from the present study are compared with previous room temperature measurements.