Environmental Science: Water Science and Technology
; Earth and Planetary Sciences: Earth-Surface Processes
; Environmental Science: Environmental Chemistry
英文摘要:
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 N2O5and HNO3that 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 NOxmolecules. During spring time, nitrate formation via the N2O5pathway is dominant, resulting in higher values of both δ18O and Δ17O. In contrast, during summer, formation involving HO2/RO2radicals 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 NO2via formation of NO2and NO3 −/HNO3. Both the model results and observations suggest that for the formation of NO2from NO, the pathway via O3is more active in spring, whereas in summer the pathway via HO2/RO2radicals 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 NOxto the sampling site. � 2017 The Authors
Research Center for Environmental Changes, Academia Sinica, Taipei, Taiwan; Centre for Climate Change Research, Indian Institute of Tropical Meteorology, Pune, India; Environmental Protection Administration Executive Yuan, Taipei, Taiwan; Department of Atmospheric Sciences, National Central University, Jhongli, Taiwan; Graduate Institute of Astronomy, National Central University, Jhongli, Taiwan; Department of Physics, University of Houston, Houston, TX, United States
Recommended Citation:
Guha T,, Lin C,T,et al. Isotopic ratios of nitrate in aerosol samples from Mt. Lulin, a high-altitude station in Central Taiwan[J]. Atmospheric Environment,2017-01-01,154