EGU22-1452
https://doi.org/10.5194/egusphere-egu22-1452
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Ion-molecule reaction laboratory experiments show that iodine oxides explain CIMS atmospheric observations attributed to iodine oxoacids 

Juan Carlos Gomez Martin1, Thomas R. Lewis2,3, Alexander D. James2, John M. C. Plane2, and Alfonso Saiz-Lopez3
Juan Carlos Gomez Martin et al.
  • 1Instituto de Astrofisica de Andalucia - CSIC, Solar System Department, Granada, Spain (jc.gomez@csic.es)
  • 2School of Chemistry, University of Leeds, LS2 9JT Leeds, UK.
  • 3Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Rocasolano, CSIC, 28006, Madrid, Spain.

Iodine chemistry is a driver of new particle formation in the marine and polar boundary layer, with potential influence on cloud formation and properties. There are however conflicting views about how iodine gas-to-particle conversion proceeds. Laboratory studies indicate that iodine photooxidation yields iodine oxides, which are well-known particle precursors1. By contrast, nitrate ion chemical ionization mass spectrometry (CIMS) field and environmental chamber observations have been interpreted as evidence of nucleation of iodine oxoacids2,3. Here, we report flow tube laboratory experiments showing that iodine oxides react with nitrate core ions to generate the same ions observed by CIMS instruments. Therefore, we conclude that molecules unlikely to form in the atmosphere in the gas-phase such as iodic acid are not necessary to explain CIMS field measurements, but rather obscure their meaning, whereas iodine oxides explain the field observations and provide a thermochemically feasible mechanism to model the climatic impact of iodine-containing particles. In addition, we propose that a key iodine reservoir species such as iodine nitrate, which we observe as a product of the reaction between iodine oxides and the nitrate anion, can be also detected by CIMS in the atmosphere and has been potentially overlooked in previous field observations4.

References

1 Gómez Martín, J.C., et al. A gas-to-particle conversion mechanism helps to explain atmospheric particle formation through clustering of iodine oxides. Nat. Commun., 11, 4521, https://doi.org/10.1038/s41467-020-18252-8, 2020

2 Sipilä, M., et al. Molecular-scale evidence of aerosol particle formation via sequential addition of HIO3. Nature 537, 532–534, https://doi.org/10.1038/nature19314, 2016.

3 He et al., Role of iodine oxoacids in atmospheric aerosol nucleation, Science, 371, 589–595, https://doi.org/10.1126/science.abe0298, 2021.

4 Baccarini et al. Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions, Nat. Commun., 11, 4924, https://doi.org/10.1038/s41467-020-18551-0, 2020.

How to cite: Gomez Martin, J. C., Lewis, T. R., James, A. D., Plane, J. M. C., and Saiz-Lopez, A.: Ion-molecule reaction laboratory experiments show that iodine oxides explain CIMS atmospheric observations attributed to iodine oxoacids , EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-1452, https://doi.org/10.5194/egusphere-egu22-1452, 2022.

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