The reactions of thioformaldehyde (H 2 CS) with OH radicals and assisted by a single water molecule have been investigated using high level ab initio quantum chemistry calculations. The H 2 CS + ˙OH reaction can in principle proceed through: (1) abstraction, and (2) addition pathways. The barrier height for the addition reaction in the absence of a catalyst was found to be −0.8 kcal mol −1 , relative to the separated reactants, which has a ∼1.0 kcal mol −1 lower barrier than the abstraction channel. The H 2 CS + ˙OH reaction assisted by a single water molecule reduces the barrier heights significantly for both the addition and abstraction channels, to −5.5 and −6.7 kcal mol −1 respectively, compared to the un-catalyzed H 2 CS + ˙OH reaction. These values suggest that water lowers the barriers by ∼6.0 kcal mol −1 for both reaction paths. The rate constants for the H 2 CS⋯H 2 O + ˙OH and OH⋯H 2 O + H 2 CS bimolecular reaction channels were calculated using Canonical Variational Transition state theory (CVT) in conjunction with the Small Curvature Tunneling (SCT) method over the atmospherically relevant temperatures between 200 and 400 K. Rate constants for the H 2 CS + ˙OH reaction paths for comparison with the H 2 CS + ˙OH + H 2 O reaction in the same temperature range were also computed. The results suggest that the rate of the H 2 CS + ˙OH + H 2 O reaction is slower than that of the H 2 CS + ˙OH reaction by ∼1–4 orders of magnitude in the temperatures between 200 and 400 K. For example, at 300 K, the rates of the H 2 CS + ˙OH + H 2 O and H 2 CS + ˙OH reactions were found to be 2.2 × 10 −8 s −1 and 6.4 × 10 −6 s −1 , respectively, calculated using [OH] = 1.0 × 10 6 molecules cm −3 , and [H 2 O] = 8.2 × 10 17 molecules cm −3 (300 K, RH 100%) atmospheric conditions. Electronic structure calculations on the H 2 C(OH)S˙ product in the presence of 3 O 2 were also performed. The results show that H 2 CS is removed from the atmosphere primarily by reacting with ˙OH and O 2 to form thioformic acid, HO 2 , formaldehyde, and SO 2 as the main end products. 
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                            Improved computational modeling of the kinetics of the acetylperoxy + HO 2 reaction
                        
                    
    
            The acetylperoxy + HO 2 reaction has multiple impacts on the troposphere, with a triplet pathway leading to peracetic acid + O 2 (reaction (1a)) competing with singlet pathways leading to acetic acid + O 3 (reaction (1b)) and acetoxy + OH + O 2 (reaction (1c)). A recent experimental study has reported branching fractions for these three pathways ( α 1a , α 1b , and α 1c ) from 229 K to 294 K. We constructed a theoretical model for predicting α 1a , α 1b , and α 1c using quantum chemical and Rice–Ramsperger–Kassel–Marcus/master equation (RRKM/ME) simulations. Our main quantum chemical method was Weizmann-1 Brueckner Doubles (W1BD) theory; we combined W1BD and equation-of-motion spin-flip coupled cluster (SF) theory to treat open-shell singlet structures. Using RRKM/ME simulations that included all conformers of acetylperoxy–HO 2 pre-reactive complexes led to a 298 K triplet rate constant, k 1a = 5.11 × 10 −12 cm 3 per molecule per s, and values of α 1a in excellent agreement with experiment. Increasing the energies of all singlet structures by 0.9 kcal mol −1 led to a combined singlet rate constant, k 1b+1c = 1.20 × 10 −11 cm 3 per molecule per s, in good agreement with experiment. However, our predicted variations in α 1b and α 1c with temperature are not nearly as large as those measured, perhaps due to the inadequacy of SF theory in treating the transition structures controlling acetic acid + O 3 formation vs. acetoxy + OH + O 2 formation. 
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                            - PAR ID:
- 10422847
- Publisher / Repository:
- Royal Society of Chemistry
- Date Published:
- Journal Name:
- Faraday Discussions
- Volume:
- 238
- ISSN:
- 1359-6640
- Page Range / eLocation ID:
- 589 to 618
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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