1. Characteristics of Aerosol Water Content and Its Implication on Secondary Inorganic Aerosol Formation during Sandy Haze in an Inland City in China
- Author
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Shiting Zhai, Panru Kang, Shenbo Wang, and Ruiqin Zhang
- Subjects
aerosol water content ,chemical component ,haze ,sandy haze ,PM2.5 ,Meteorology. Climatology ,QC851-999 - Abstract
Sand events continue to occur frequently and affect the North China region. Under unfavorable meteorological conditions, they can easily combine with haze pollution, forming sandy haze events that have a significant impact on human health. Aerosol water content (AWC) is known to have a significant impact on PM2.5, but its effect is still unclear in sandy haze. In this work, sandy haze and haze periods were observed in Zhengzhou using a series of high-time-resolution instruments. The AWC calculated by the ISORROPIA-II model reached 11 ± 5 μg m−3, accounting for 10% of the PM2.5, in the sandy haze period. Sensitivity tests show that AWC was mainly relative humidity (RH)-dependent. Additionally, elevated SO42−, TNO3, and TNH4 were crucial in the increase in AWC. The increase in Ca2+ ions in the sandy haze led to lower AWC than that in the haze periods. Specifically, (NH4)2SO4 was the major contributor to the AWC when the RH was between 30 and 46% in the sandy haze period, and NH4NO3 gradually became the main contributor with the increase in RH. In turn, AWC could enhance the formation of sulfate and nitrate, even during the sandy haze period. Therefore, the emergency control of gaseous precursors should also be implemented before the sand events.
- Published
- 2024
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