Seasonal variation and secondary formation of size-segregated aerosol water-soluble inorganic ions in a coast megacity of North China Plain

被引:10
|
作者
Yao, Qing [1 ]
Liu, Zirui [2 ]
Han, Suqin [1 ]
Cai, Ziying [1 ]
Liu, Jingle [3 ]
Hao, Tianyi [1 ]
Liu, Jinyun [2 ]
Huang, Xiaojuan [2 ]
Wang, Yuesi [2 ,4 ,5 ]
机构
[1] Tianjin Environm Meteorol Ctr, CMA NKU Cooperat Lab Atmospher Environm Hlth Res, Tianjin 300074, Peoples R China
[2] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing 100029, Peoples R China
[3] Tianjin Meteorol Inst, Tianjin 300074, Peoples R China
[4] Chinese Acad Sci, Ctr Excellence Reg Atmospher Environm, Inst Urban Environm, Xiamen 361021, Peoples R China
[5] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
Water-soluble inorganic ions; Size distribution; Seasonal variation; Secondary formation; Tianjin; BIOMASS BURNING CONTRIBUTION; FINE PARTICULATE MATTER; CHEMICAL-COMPOSITIONS; SOURCE APPORTIONMENT; HYGROSCOPIC GROWTH; SUBMICRON AEROSOLS; ORGANIC AEROSOLS; RIVER-DELTA; PM2.5; PM10;
D O I
10.1007/s11356-020-09052-0
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The aerosol samples of water-soluble inorganic ions (WSIs), including SO42-, NO3-, NH4+, Cl-, K+, Na+, Ca2+, and Mg2+ in size-segregated particulate matter (PM), were collected by an Anderson sampler (with 8 nominal cut-sizes ranged from 0.43 to 9.0 mu m) in urban Tianjin during 2013-2014. The results showed that particulate matters in the fine mode (PM2.1, Dp < 2.1 mu m) comprised large part of mass concentrations of aerosols, and the water-soluble ionic species in the fine mode were 47.07 +/- 14.29 mu g m(-3) (spring), 67.87 +/- 28.74 mu g m(-3) (summer), 86.60 +/- 48.53 mu g m(-3) (autumn), and 104.16 +/- 51.76 mu g m(-3) (winter), respectively, which accounted for 59.5%, 63.3%, 71.9%, and 71.4% of the PM2.1 mass concentrations. Secondary pollutants of SO42-, NO3-, and NH4+ (SNA) were the dominant contributors of WSIs, which showed a bimodal size distribution in each season, with the larger peak appeared in the size fraction of 0.65-1.1 mu m and the smaller one in 3.3-5.8 mu m fraction. SNA concentrations in lightly polluted days (LPD) and heavily polluted days (HPD) were observably higher than non-polluted days (NPD), especially in the fine mode, with the peak diameter moving from 0.43-0.65 mu m on NPD to 0.65-1.1 mu m on LPD and HPD. The correlation analysis between NH4+, NO3-, and SO42- suggested that almost all SO42- and NO3- for fine particles had been completely neutralized by NH4+, and primarily existed in the forms of (NH4)(2)SO4 and NH4NO3. The sulfur oxidation ratio (SOR) and nitrogen oxidation ratio (NOR) on LPD and HPD in fine mode were observably higher than those on NPD, especially in the range of 0.65-1.1 mu m and 1.1-2.1 mu m. Furthermore, SOR and NOR values in the size fraction of 0.43-3.3 mu m increase as the RH elevated, especially in 0.43-2.1 mu m, where RH was significantly positive correlated with SOR and NOR, indicating the significant contributions of heterogeneous processes to the secondary formation of SO42- and NO3-. These results suggested an enhanced formation ability of secondary pollutants under high RH in the coast city. Therefore, controlling the precursors of SNA, such as SO2 and NOx, would be more effective to reduce the fine particulate pollution in the coast megacity of Tianjin.
引用
收藏
页码:26750 / 26762
页数:13
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