Abstract
In autumn of 2008, the chemical characteristics of major secondary ionic aerosols at a suburban site in central Taiwan were measured during an annually occurring season of high pollution. The semicontinuous measurement system measured major soluble inorganic species, including NH4+, NO3−, and SO42−, in PM10 with a 15 min resolution time. The atmospheric conditions, except for the influences of typhoons, were dominated by the local sea-land breeze with clear diurnal variations of meteorological parameters and air pollutant concentrations. To evaluate secondary aerosol formation at different ozone levels, daily ozone maximum concentration (O3,daily max) was used as an index of photochemical activity for dividing between the heavily polluted period (O3,daily max ≧80 ppb) and the lightly polluted period (O3,daily max<80 ppb). The concentrations of PM10, NO3−, SO42−, NH4+ and total major ions during the heavily polluted period were 1.6, 1.9, 2.4, 2.7 and 2.3 times the concentrations during the lightly polluted period, respectively. Results showed that the daily maximum concentrations of PM10 occurred around midnight and the daily maximum ozone concentration occurred during daytime. The average concentration of SO2 was higher during daytime, which could be explained by the transportation of coastal industry emissions to the sampling site. In contrast, the high concentration of NO2 at night was due to the land breeze flow that transport inland urban air masses toward this site. The simulations of breeze circulations and transitions were reflected in transports and distributions of these pollutants. During heavily polluted periods, NO3− and NH4+ showed a clear diurnal variations with lower concentrations after midday, possibly due to the thermal volatilization of NH4NO3 during daytime and transport of inland urban plume at night. The diurnal variation of PM10 showed the similar pattern to that of NO3− and NH4+ aerosols. This indicated that the formatted secondary aerosols in the inland urban area could be transported to the coastal area by the weak land breeze and deteriorated the air quality in the coastal area at night.
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