Diurnal variations in oxygen and nitrogen isotopes of atmospheric nitrogen dioxide and nitrate: implications for tracing NOx oxidation pathways and emission sources.

The oxygen (Δ17 O) and nitrogen (δ15 N) isotopic compositions of atmospheric nitrate (NO 3-) are widely used as tracers of its formation pathways, precursor (nitrogen oxides (NO x) ≡ nitric oxide (NO) + nitrogen dioxide (NO 2)) emission sources, and physico-chemical processing. However, the lack of observations on the multi-isotopic composition of NO 2 perpetuates significant uncertainties regarding the quantitative links between the isotopic composition of NO x and NO 3- , which ultimately may bias inferences about NO 3- formation processes and the distribution of sources, particularly in winter urban atmospheres. We report here on the first simultaneous atmospheric observations of Δ17 O and δ15 N in NO 2 (n=16) and NO 3- (n=14). The measurements were carried out at sub-daily (∼3 h) resolution over 2 non-consecutive days in an Alpine city in February 2021. A strong diurnal signal is observed in both NO 2 and NO 3- multi-isotopic composition. Δ17 O of NO 2 and NO 3- ranges from 19.6 ‰ to 40.8 ‰ and from 18.3 ‰ to 28.1 ‰, respectively. During the day and night, the variability in Δ17 O(NO 2) is mainly driven by the oxidation of NO by ozone, with a substantial contribution from peroxy radicals in the morning. NO 3- mass balance equations, constrained by observed Δ17 O(NO 2), suggest that during the first day of sampling, most of the NO 3- was formed locally from the oxidation of NO 2 by hydroxyl radicals by day and via heterogeneous hydrolysis of dinitrogen pentoxide at night. For the second day, calculated and observed Δ17 O(NO 3-) do not match, particularly daytime values; the possible effects on Δ17 O(NO 3-) of a Saharan dust event that occurred during this sampling period and of winter boundary layer dynamics are discussed. δ15 N of NO 2 and NO 3- ranges from - 10.0 ‰ to 19.7 ‰ and from - 4.2 ‰ to 14.9 ‰, respectively. Consistent with theoretical predictions of N isotope fractionation, the observed variability in δ15 N(NO 2) is explained by significant post-emission equilibrium N fractionation. After accounting for this effect, vehicle exhaust is found to be the primary source of NO x emissions at the sampling site. δ15 N(NO 3-) is closely linked to δ15 N(NO 2) variability, bringing further support to relatively fast and local NO x processing. Uncertainties in current N fractionation factors during NO 2 to NO 3- conversion are underlined. Overall, this detailed investigation highlights the potential and necessity of simultaneously using Δ17 O and δ15 N in NO 2 and NO 3- in order to better constrain quantitative inferences about the sources and formation chemistry of NO 3- in urban environments in winter. [ABSTRACT FROM AUTHOR]