Measurement of Henry's law and liquid-phase loss rate constants of peroxypropionic nitric anhydride (PPN) in deionized water and in n-octanol
-
Published:2023-01-10
Issue:1
Volume:23
Page:311-322
-
ISSN:1680-7324
-
Container-title:Atmospheric Chemistry and Physics
-
language:en
-
Short-container-title:Atmos. Chem. Phys.
Author:
Easterbrook Kevin D., Vona Mitchell A., Nayebi-Astaneh Kiana, Miller Amanda M., Osthoff Hans D.ORCID
Abstract
Abstract. The Henry's law solubility (HS) and liquid-phase loss rate constants (kl) of the tropospheric trace gas constituents
peroxyacetic nitric anhydride (PAN; CH3C(O)O2NO2, commonly known as peroxyacetyl nitrate) and peroxypropionic nitric
anhydride (PPN; C2H5C(O)O2NO2, also known as peroxypropionyl nitrate) in deionized (DI) water and of PPN in n-octanol
were measured using a flow bubble apparatus at temperatures between 5.0 and 25.0 ∘C. For PAN in DI water, the observed values
for HS,aq are consistent with the literature, whereas the solubility of PPN in DI water is slightly lower than literature
values, ranging from HScp(PPN)aq = (1.49 ± 0.05) M atm−1 at 25.0 ∘C to
HScp(PPN)aq = (7.01 ± 0.25) M atm−1 at 5.0 ∘C (stated uncertainties are
at the 1σ level). The data are best described by
ln(HScp(PAN)aq/[Matm-1]) = -(17.8±0.3) + (5620±85)/T and
ln(HScp(PPN)aq/[Matm-1]) = -(19.5±1.7) + (5955±480)/T, where T is in
kelvin. For n-octanol, the PPN solubility ranges from
HScp(PPN)oct = (88±5)Matm-1 at 25.0 ∘C to
HScpoct = (204±16)Matm-1 at 5.0 ∘C and is best described by
ln(HScp(PPN)oct/[Matm-1]) = -(6.92±0.75) + (3390±320)/T. n-Octanol–water
partition coefficients (KOW) for PPN were determined for the first time, ranging from 59 ± 4 at 25.0 ∘C to
29 ± 3 at 5.0 ∘C. Observed loss rate constants in DI water are consistent with recent literature and larger than the thermal
dissociation rates for both PAN and PPN, consistent with a hydrolysis mechanism, whereas kl values in n-octanol are
significantly smaller than gas-phase dissociation rate constants, likely owing to a “cage effect” in the organic liquid. The results imply that
uptake of either PAN or PPN on cloud water and organic aerosol is negligible but that uptake of PPN may constitute an
overlooked source of peroxy radicals in organic aerosol.
Funder
Natural Sciences and Engineering Research Council of Canada
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference47 articles.
1. Burkholder, J. B., Sander, S. P., Abbatt, J., Barker, J. R., Cappa, C., Crounse, J. D., Dibble, T. S., Huie, R. E., Kolb, C. E.,
Kurylo, M. J., Orkin, V. L., Percival, C. J., Wilmouth, D. M., and Wine, P. H.: Chemical Kinetics and Photochemical
Data for Use in Atmospheric Studies, Evaluation No. 19, JPL Publication 19-5, Jet Propulsion Laboratory, Pasadena, http://jpldataeval.jpl.nasa.gov (last access: 5 January 2021),
2019. 2. Davidovits, P., Kolb, C. E., Williams, L. R., Jayne, J. T., and Worsnop, D. R.:
Mass accommodation and chemical reactions at gas-liquid interfaces, Chem. Rev., 106, 1323–1354, https://doi.org/10.1021/cr040366k, 2006. 3. Frenzel, A., Kutsuna, S., Takeuchi, K., and Ibusuki, T.:
Solubility and reactivity of peroxyacetyl nitrate (PAN) in dilute aqueous salt solutions and in sulphuric acid, Atmos. Environ., 34, 3641–3644, https://doi.org/10.1016/S1352-2310(00)00132-1, 2000. 4. Furgeson, A., Mielke, L. H., Paul, D., and Osthoff, H. D.:
A photochemical source of peroxypropionic and peroxyisobutanoic nitric anhydride, Atmos. Environ., 45, 5025–5032, https://doi.org/10.1016/j.atmosenv.2011.03.072, 2011. 5. Gaffney, J. S. and Marley, N. A.:
The Impacts of Peroxyacetyl Nitrate in the Atmosphere of Megacities and Large Urban Areas: A Historical Perspective, ACS Earth Space Chem., 5, 1829–1841, https://doi.org/10.1021/acsearthspacechem.1c00143, 2021.
Cited by
3 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|