Abstract

Ozonolysis of alkenes is a key reaction in the atmosphere, playing an important role in determining the oxidising capacity of the atmosphere and acting as a source of compounds that can contribute to local photochemical “smog”. The reaction products of the initial step of alkene-ozonolysis are Criegee intermediates (CIs), which have for many decades eluded direct experimental detection because of their very short lifetime. We use an innovative experimental technique, stabilisation of CIs with spin traps and analysis with proton transfer reaction mass spectrometry, to measure the gas phase concentration of a series of CIs formed from the ozonolysis of a range of both biogenic and anthropogenic alkenes in flow tube experiments. Density functional theory (DFT) calculations were used to assess the stability of the CI-spin trap adducts and show that the reaction of the investigated CIs with the spin trap occurs very rapidly except for the large β-pinene CI. Our measurement method was used successfully to measure all the expected CIs, emphasising that this new technique is applicable to a wide range of CIs with different molecular structures that were previously unidentified experimentally. In addition, for the first time it was possible to study CIs simultaneously in an even more complex reaction system consisting of more than one olefinic precursor. Comparison between our new experimental measurements, calculations of stability of the CI-spin trap adducts and results from numerical modelling, using the master chemical mechanism (MCM), shows that our new method can be used for the quantification of CIs produced in situ in laboratory experiments.

Highlights

  • The Anthropocene has seen huge changes in the composition of the atmosphere

  • This method was successfully applied to the measurement of Criegee Intermediates (CIs) from the ozonolysis of a-pinene, the structure of the CI-spin trap adduct was characterised in detail and we showed the potential of this technique to be used for quanti cation purposes.[18]

  • We compared the experimentally measured concentrations of CI–dimethyl-pyrroline N-oxide (DMPO) adducts with those expected from numerical modelling, using the AtChem/MCM model

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Summary

Introduction

The Anthropocene has seen huge changes in the composition of the atmosphere. Volatile organic compounds (VOCs) play an important role in determining the overall composition and reactivity of the atmosphere. Many VOC sources have signi cantly changed since the onset of the Anthropocene in strength but new sources and VOCs have emerged. Oxidative degradation in the atmosphere with oxidants such as ozone is one of the main removal processes for VOCs. Ole nic VOCs react strongly with ozone leading to a complex reaction scheme with a large number of stable and reactive intermediate reaction products. The initial step of alkene–ozone reactions is a 1,3-cycloaddition to produce a molozonide, which subsequently decomposes to produce so-called Criegee Intermediates (CIs) and a carbonyl product. In the condensed phase a further rearrangement is possible, but this is not the case in the gas phase.[1,2,3]

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