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Published on: June 14, 2018
Post-Transition-State Direct Dynamics Simulations on the Ozonolysis of Catechol
Ankita Agarwal1, Palash Jyoti Boruah1, Biplab Sarkar2
1Department of Chemistry, National Institute of Technology Meghalaya, Shillong 793003, Meghalaya, India.
On-the-fly dynamics simulations reveal catechol + ozone reactions form peroxyacids that fragment into CO, CO2, H2O, and SCA. Reaction rates and product branching ratios were calculated and compared with experimental data.
Area of Science:
- Atmospheric Chemistry
- Chemical Kinetics
- Computational Chemistry
Background:
- Catechol and ozone reactions are significant in atmospheric chemistry.
- Understanding reaction pathways and product distributions is crucial for atmospheric modeling.
Purpose of the Study:
- To investigate the on-the-fly dynamics of the catechol + ozone reaction.
- To elucidate the post-transition state dynamics and product formation channels.
- To calculate reaction rates and branching ratios for comparison with experimental data.
Main Methods:
- On-the-fly dynamics simulations were performed.
- The PM7 semiempirical method was used to calculate potential energy gradients.
- Hamilton's equations of motion were integrated.
- Calculated results were validated against high-level ab initio methods (B3LYP/6-311+G (2df, 2p)).
Main Results:
- The reaction proceeds via a peroxyacid intermediate, followed by dissociation into various fragments.
- Four major product channels were identified: CO, CO2, H2O, and small carboxylic acid (SCA).
- Reaction rates and product branching ratios were computed at 400 K and 500 K.
- Minimum energy profiles and qualitative activation energies for key channels were determined.
Conclusions:
- The study provides detailed insights into the reaction mechanism and dynamics of catechol + ozone.
- Calculated branching ratios show good agreement with experimental observations.
- The findings contribute to a better understanding of atmospheric oxidation processes involving phenolic compounds.
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