[Characteristics of the Size Distribution of Water-soluble Ions During a Heavy Pollution Episode in the Winter in Tianjin].

Huan Jing Ke Xue

State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry(LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China.

Published: December 2017

To characterize the size distribution of water-soluble inorganic ions (WSⅡ) during a heavy pollution episode, particle samples were collected by an Andersen cascade sampler in Tianjin in January 2014, and the concentrations of eight WSⅡ (Na, NH, K, Mg, Ca, Cl, NO, and SO) during a typical haze episode were analyzed by ion chromatography. The sources and formation mechanisms of WSⅡ were analyzed based on their size distributions. The results showed that the daily average concentrations of PM and PM were (138±100) μg·m and (227±142) μg·m, respectively, and the average concentration of total WSⅡ concentrations (TWSⅡ) in the coarse and fine particles were (34.07+6.16) μg·m and (104.16+51.76) μg·m, respectively. The concentrations of SO, NO, and NH in the fine particles were much higher than concentrations of the other ions, and there were strong correlations between these three ions. The TWSⅡ on clear days, light pollution days, and heavy pollution days were (41.55±12.41) μg·m, (94.46±31.19) μg·m, and (147.55±27.76) μg·m, respectively. On clear days, SO showed a unimodal distribution, peaking at 0.43-0.65 μm; and NO showed a trimodal distribution, peaking at 0.43-0.65 μm, 2.1-3.3 μm, and 5.8-9.0 μm. NH had a bimodal distribution, peaking at 0.43-0.65 μm and 4.7-5.8 μm. On heavy pollution days, however, the size distributions of these three secondary inorganic ions switched to a unimodal size distribution, peaking at 0.65-1.1 μm. Unimodal NH mainly coexisted with SO and NO, and the excess NH was found to be combined with Cl in the fine particles. In the coarse particles, NH completely coexisted with SO and NO.

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http://dx.doi.org/10.13227/j.hjkx.201702097DOI Listing

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