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Updated: Sep 22, 2025

Computation of Atmospheric Concentrations of Molecular Clusters from ab initio Thermochemistry
Published on: April 8, 2020
Hydrotrioxide (ROOOH) formation in the atmosphere
Torsten Berndt1, Jing Chen2, Eva R Kjærgaard2
1Atmospheric Chemistry Department (ACD), Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany.
Atmospheric organic hydrotrioxides (ROOOH) are directly observed forming from organic peroxy radicals (RO2) and hydroxyl radicals (OH). This previously overlooked substance class has a significant global formation yield and short atmospheric lifetime.
Area of Science:
- Atmospheric Chemistry
- Organic Chemistry
- Environmental Science
Background:
- Organic hydrotrioxides (ROOOH) are potent oxidants utilized in organic synthesis.
- Previous speculation suggested atmospheric formation via gas-phase reactions between organic peroxy radicals (RO2) and hydroxyl radicals (OH).
Purpose of the Study:
- To directly observe the formation of organic hydrotrioxides (ROOOH) in the atmosphere.
- To investigate the kinetics of the RO2 + OH reaction.
- To quantify the atmospheric formation yield and impact of ROOOH.
Main Methods:
- Direct observation of ROOOH formation from atmospherically relevant RO2 radicals.
- Kinetic analysis of RO2 + OH reactions.
- Global modeling of isoprene degradation to predict ROOOH yields.
Main Results:
- Direct observation confirmed ROOOH formation from RO2 + OH reactions.
- Reaction rate coefficients were found to be near the collision limit.
- Global modeling predicted up to 1% molar hydrotrioxide yields from isoprene degradation, totaling ~10 million metric tons annually.
- Estimated atmospheric lifetime of ROOOH is minutes to hours.
Conclusions:
- Organic hydrotrioxides (ROOOH) are a newly identified, significant class of atmospheric compounds.
- The rapid formation and substantial yield necessitate further examination of their atmospheric impact.
- ROOOH represent a previously omitted component in atmospheric chemistry models.
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