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Electron-triggered chemistry in HNO(3)/H(2)O complexes

Polar stratospheric clouds, which consist mainly of nitric acid containing ice particles, play a pivotal role in stratospheric chemistry. We investigate mixed nitric acid–water clusters (HNO(3))(m)(H(2)O)(n), m ≈ 1–6, n ≈ 1–15, in a laboratory molecular beam experiment using electron attachment and...

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Detalles Bibliográficos
Autores principales: Lengyel, Jozef, Ončák, Milan, Fedor, Juraj, Kočišek, Jaroslav, Pysanenko, Andriy, Beyer, Martin K., Fárník, Michal
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Royal Society of Chemistry 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5450009/
https://www.ncbi.nlm.nih.gov/pubmed/28397887
http://dx.doi.org/10.1039/c7cp01205e
Descripción
Sumario:Polar stratospheric clouds, which consist mainly of nitric acid containing ice particles, play a pivotal role in stratospheric chemistry. We investigate mixed nitric acid–water clusters (HNO(3))(m)(H(2)O)(n), m ≈ 1–6, n ≈ 1–15, in a laboratory molecular beam experiment using electron attachment and mass spectrometry and interpret our experiments using DFT calculations. The reactions are triggered by the attachment of free electrons (0–14 eV) which leads to subsequent intracluster ion–molecule reactions. In these reactions, the nitrate anion NO(3) (–) turns out to play the central role. This contradicts the electron attachment to the gas-phase HNO(3) molecule, which leads almost exclusively to NO(2) (–). The nitrate containing clusters are formed through at least three different reaction pathways and represent terminal product ions in the reaction cascade initiated by the electron attachment. Besides, the complex reaction pathways represent a new hitherto unrecognized source of atmospherically important OH and HONO molecules.