Isotopic ratios of nitrate in aerosol samples from Mt. Lulin, a high-altitude station in Central Taiwan

Publication date: April 2017
Source:Atmospheric Environment, Volume 154
Author(s): Tania Guha, C.T. Lin, S.K. Bhattacharya, A.S. Mahajan, Chang-Feng Ou-Yang, Yi-Ping Lan, S.C. Hsu, Mao-Chang Liang
The importance of Asian countries towards increase of atmospheric pollutants is being examined critically in recent times. In this context, we carried out analysis of nitrates separated from aerosol samples collected during 2010 from Mt. Lulin (NOAA code: LLN), Taiwan, located at an altitude of 2 862 m above sea level. Large temporal variations are seen in δ¹⁵N, δ¹⁸O and Δ¹⁷O values of the nitrate, with day-to-day variations comparable to the seasonal amplitude. The δ¹⁵N values of nitrate are found to be higher in spring months (March–April; −1±3‰) and lower in summer (June–September; −5±3‰). Similarly, the δ¹⁸O (69 ± 15‰ versus 32 ± 13‰) and Δ¹⁷O (23 ± 5‰ versus 12 ± 4‰) values are higher in spring and lower in summer. The lowest δ¹⁸O value observed was 10.8‰. The higher values of δ¹⁵N in spring could be attributed to enhanced contribution from fossil fuel combustions, especially burning of coal in nearby Asian countries like China, with the resultant pollutants being brought to the Lulin station by long-range transport. An alternative explanation is the isotopic exchange reaction between N2O5 and HNO3 that elevates the δ¹⁵N value in nitrate. The oxygen isotope variability is explained by changes in contribution from two major pathways of nitrate formation from its precursor NOx molecules. During spring time, nitrate formation via the N2O5 pathway is dominant, resulting in higher values of both δ¹⁸O and Δ¹⁷O. In contrast, during summer, formation involving HO2/RO2 radicals becomes important, producing lower values of δ¹⁸O and Δ¹⁷O. A chemistry box model was used to study the nitrate formation pathways through oxidation of NO and NO2 via formation of NO2 and NO3⁻/HNO3. Both the model results and observations suggest that for the formation of NO2 from NO, the pathway via O3 is more active in spring, whereas in summer the pathway via HO2/RO2 radicals predominates. For the subsequent formation of NO3⁻ and HNO3, the OH pathway is more active in summer than in spring. These suggestions are supported by a wind rose diagram and back trajectory analysis of air masses bringing the precursor NOx to the sampling site.



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