Heterogeneous Reactions of N <sub>2</sub> O <sub>5</sub> with Nitrate- and Chloride-Containing Solutions: Isotopic Evidence for the Nitration of N <sub>2</sub> O <sub>5</sub>
The nitrate (NO<sub>3</sub><sup>-</sup>) ion has been shown to suppress the reactive uptake of dinitrogen pentoxide (N<sub>2</sub>O<sub>5</sub>) to aqueous aerosol, yet a molecular mechanism that explains this effect remains elusive. To explore how N<sub>2</sub>O<sub>5</sub> and NO<sub>3</sub><sup>-</sup> interact in solution, we use isotopically labeled <sup>15</sup>NO<sub>3</sub><sup>-</sup> in the presence of Cl<sup>-</sup> to mark <sup>14,14</sup>N<sub>2</sub>O<sub>5</sub> that react with <sup>15</sup>NO<sub>3</sub><sup>-</sup> by detecting the nitration and chlorination products <sup>14,15</sup>N<sub>2</sub>O<sub>5</sub>, <sup>15,15</sup>N<sub>2</sub>O<sub>5</sub>, Cl<sup>14</sup>NO<sub>2,</sub> and Cl<sup>15</sup>NO<sub>2</sub>. At three Na<sup>15</sup>NO<sub>3</sub> concentrations (0.47, 1.35, and 3.7 M), both Cl<sup>14</sup>NO<sub>2</sub> and Cl<sup>15</sup>NO<sub>2</sub> products are measured as the NaCl concentration increases from 0 to 3.0 M, confirming that N<sub>2</sub>O<sub>5</sub> can reactively exchange with NO<sub>3</sub><sup>-</sup> prior to chlorination. Using a kinetic multilayer model to compare chlorination and nitration (nitrate exchange) of N<sub>2</sub>O<sub>5</sub>, the rate constant ratio <i>k</i><sub>Cl<sup>-</sup></sub><i>/k</i><sub>NO<sub>3</sub><sup>-</sup></sub> is determined to be between 2 and 6 for the three <sup>15</sup>NO<sub>3</sub><sup>-</sup> concentrations. Model results suggest that the initial adsorption of a <sup>14,14</sup>N<sub>2</sub>O<sub>5</sub> molecule produces the majority of Cl<sup>15</sup>NO<sub>2</sub> by exchange with <sup>15</sup>NO<sub>3</sub><sup>-</sup> before reacting with Cl<sup>-</sup>, rather than occurring through multiple absorption and evaporation events involving <sup>14,15</sup>N<sub>2</sub>O<sub>5</sub> or <sup>15,15</sup>N<sub>2</sub>O<sub>5</sub>. The ratio of nitrate exchange to hydrolysis, <i>k</i><sub>NO<sub>3</sub><sup>-</sup></sub><i>/k</i><sub>H<sub>2</sub>O</sub>, is inferred to be between 70 and 230, which overestimates nitrate suppression in 6 M NaNO<sub>3</sub> by 10-fold when using previous parametrizations of N<sub>2</sub>O<sub>5</sub> uptake based on an S<sub>N</sub>1 NO<sub>2</sub><sup>+</sup> mechanism. We propose an alternate S<sub>N</sub>2 mechanism involving N<sub>2</sub>O<sub>5</sub> activation and deactivation that fits both isotope and uptake data.
Authors
- Steven J. Kregel (ORCID: https://orcid.org/0000-0001-5712-829X)
- Thomas F. Derrah (ORCID: https://orcid.org/0000-0003-4110-9005)
- Gilbert M. Nathanson (ORCID: https://orcid.org/0000-0002-6921-6841)
- Manabu Shiraiwa (ORCID: https://orcid.org/0000-0003-2532-5373)
- Timothy H. Bertram (ORCID: https://orcid.org/0000-0002-3026-7588)
- Pascale S. J. Lakey (ORCID: https://orcid.org/0000-0003-2923-4073)
Institutions
- University of Wisconsin–Madison (US)
- University of California, Irvine (US)
- Irvine University (US)
Publication Details
- Journal
- The Journal of Physical Chemistry A
- Published
- 2025-11-10
- DOI
- https://doi.org/10.1021/acs.jpca.5c06048
- Primary Topic
- Atmospheric chemistry and aerosols
- Type
- article
- Field-Weighted Citation Impact
- 0.00