| Literature DB >> 28397887 |
Jozef Lengyel1, Milan Ončák, Juraj Fedor, Jaroslav Kočišek, Andriy Pysanenko, Martin K Beyer, Michal Fárník.
Abstract
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 (HNO3)m(H2O)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 NO3- turns out to play the central role. This contradicts the electron attachment to the gas-phase HNO3 molecule, which leads almost exclusively to NO2-. 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.Entities:
Year: 2017 PMID: 28397887 PMCID: PMC5450009 DOI: 10.1039/c7cp01205e
Source DB: PubMed Journal: Phys Chem Chem Phys ISSN: 1463-9076 Impact factor: 3.676
Fig. 1Panels (a and c): cumulative negative ion mass spectra for (HNO3)(H2O) cluster beam and gas-phase HNO3, respectively. Panel (b): cluster beam spectral analysis distinguishing different groups of mass peaks. The cluster beam spectrum was obtained as a sum of all the mass spectra in the energy range 0–14 eV with an energy step of 0.25 eV. It was normalized to the most intense cluster ion HNO3NO3 – (m/z = 125), the NO2 – peak (intensity of 3.5) is omitted from the figure for clarity. The gas-phase spectrum represents a sum of the mass spectra in the same energy range with a step of 0.05 eV, normalized to the NO2 – peak.
Fig. 2Reaction energies of various dissociation channels after electron attachment to (HNO3)(H2O) clusters, m = 1–3, n = 0–5, calculated at the M06-2X/aug-cc-pVDZ level of theory.
Energy of evaporation (in eV) of H2O, HONO, and HNO3 from clusters formed after OH dissociation and internal rearrangement to form HONO. Calculated at the M06-2X/aug-cc-pVDZ level of theory
| Ion | Evaporating molecule |
| |||||
| 0 | 1 | 2 | 3 | 4 | 5 | ||
| HONO(H2O) | H2O | — | 0.48 | 0.37 | 0.41 | 0.64 | 0.45 |
| HONO | 1.00 | 0.85 | 0.68 | 0.60 | 0.78 | 0.79 | |
| HONO(H2O) | H2O | — | 0.54 | 0.23 | 0.67 | 0.40 | 0.46 |
| HONO | 0.50 | 0.66 | 0.51 | 0.70 | 0.54 | 0.51 | |
| HNO3 | 0.95 | 1.00 | 0.86 | 1.12 | 0.88 | 0.89 | |
Fig. 3Schematic illustration of reaction pathways observed in electron attachment to mixed (HNO3)(H2O) clusters.