Experimental Kinetic Study of the Reactions of Atomic Chlorine with H2S, SH, and OCS

Abstract The reactions of Cl atoms with H2S, SH, and OCS, of interest for atmospheric chemistry, were studied at a total pressure of 2 Torr as a function of temperature in a low-pressure discharge flow-tube reactor with mass spectrometric detection of the species involved. The rate constants of the reactions Cl + H2S → SH + HCl (1) and Cl + OCS → SCl + CO (3) were determined under pseudo-first-order conditions, monitoring the kinetics of consumption of chlorine atoms under conditions of excess molecular reagent: k1 = (3.72 ± 0.08) × 10–11 exp((209 ± 7)/T) cm3 molecule–1 s–1 (T = 220–960 K) and k3 = (2.6 ± 1.5) × 10–10 exp(−(8440 ± 520)/T) cm3 molecule–1 s–1 (T = 755–1000 K), with estimated total uncertainties of 15% and 20%, respectively, at all temperatures. The rate constant of chlorine atoms with SH, an important intermediate in the oxidation of sulfur-containing compounds, Cl + SH → S + HCl (2), was determined at T = 220–960 K by monitoring the kinetics of the SH radical in reaction (1) carried out in excess of Cl atoms: k2 = (1.23 ± 0.03) × 10–10 exp((90 ± 9)/T) cm3 molecule–1 s–1, with a conservative (temperature-independent) uncertainty of 20%. The kinetic data from the present study are compared with previous measurements and theoretical calculations.

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Publication Details

Journal
ACS Earth and Space Chemistry
Published
2026-10-16
DOI
https://doi.org/10.1021/acsearthspacechem.6c00276
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
0.00

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article

Experimental Kinetic Study of the Reactions of Atomic Chlorine with H2S, SH, and OCS

Yuri Bedjanian
ACS Earth and Space Chemistry
Atmospheric chemistry and aerosols
article

Experimental Kinetic Study of the Reactions of Atomic Chlorine with H2S, SH, and OCS

Yuri Bedjanian
article en

Abstract

Abstract The reactions of Cl atoms with H2S, SH, and OCS, of interest for atmospheric chemistry, were studied at a total pressure of 2 Torr as a function of temperature in a low-pressure discharge flow-tube reactor with mass spectrometric detection of the species involved. The rate constants of the reactions Cl + H2S → SH + HCl (1) and Cl + OCS → SCl + CO (3) were determined under pseudo-first-order conditions, monitoring the kinetics of consumption of chlorine atoms under conditions of excess molecular reagent: k1 = (3.72 ± 0.08) × 10–11 exp((209 ± 7)/T) cm3 molecule–1 s–1 (T = 220–960 K) and k3 = (2.6 ± 1.5) × 10–10 exp(−(8440 ± 520)/T) cm3 molecule–1 s–1 (T = 755–1000 K), with estimated total uncertainties of 15% and 20%, respectively, at all temperatures. The rate constant of chlorine atoms with SH, an important intermediate in the oxidation of sulfur-containing compounds, Cl + SH → S + HCl (2), was determined at T = 220–960 K by monitoring the kinetics of the SH radical in reaction (1) carried out in excess of Cl atoms: k2 = (1.23 ± 0.03) × 10–10 exp((90 ± 9)/T) cm3 molecule–1 s–1, with a conservative (temperature-independent) uncertainty of 20%. The kinetic data from the present study are compared with previous measurements and theoretical calculations.

ACS Earth and Space Chemistry
Institut de Combustion Aérothermique Réactivité et Environnement (FR)
Agence Nationale de la Recherche
Openalex Percentile: Top 20%
Atmospheric chemistry and aerosols
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