Concentration, Size Distribution, and Formation of Trimethylaminium and Dimethylaminium Ions in Atmospheric Particles over Marginal Seas of China*

被引:30
|
作者
Hu, Qingjing [1 ]
Yu, Peiran [1 ]
Zhu, Yujiao [1 ]
Li, Kai [1 ]
Gao, Huiwang [1 ]
Yao, Xiaohong [1 ,2 ]
机构
[1] Ocean Univ China, Key Lab Marine Environm Sci & Ecol, Minist Educ, Qingdao 266100, Peoples R China
[2] Qingdao Collaborat Innovat Ctr Marine Sci & Techn, Qingdao, Peoples R China
基金
中国国家自然科学基金;
关键词
ALIPHATIC-AMINES; CHLORIDE DEPLETION; ARABIAN SEA; AEROSOL; GAS; METHYLAMINES; AMMONIUM; PHASE; FOG; SPECIATION;
D O I
10.1175/JAS-D-14-0393.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In this paper, the concentration, the size distribution, and the formation of dimethylaminium (DMA(+)) and trimethylaminium (TMA(+)) ions in atmospheric particles were studied during a cruise campaign over the Yellow Sea and the Bohai Sea of China in May 2012. The concentrations of DMA(+) and TMA(+) in particles smaller than 11 mu m were 4.4 +/- 3.7 and 7.2 +/- 7.1 nmol m(-3), respectively. The two ions had a good correlation (R-2 = 0.86), and both had a moderately good correlation with chlorophyll a fluorescence (R-2 = 0.66-0.67). The observed concentrations were from one to three orders of magnitude larger than the concentrations reported in other marine atmospheres. They were also much larger than the values observed at a coastal site neighboring the Yellow Sea in May-June 2013. The high concentrations of DMA(+) and TMA(+) observed in the marine atmosphere were probably associated with local biogenic activity instead of the long-range transport of these species from adjacent continents. The calculated mole ratios of (DMA(+) + TMA(+)) to [GRAPHICS] in different-sized particles over the seas indicated that (DMA(+) + TMA(+)) most likely played an important role in neutralizing acidic species in particles less than 0.43 mu m but not in particles of other sizes. Size distributions of DMA(+) and TMA(+) in the marine and coastal atmospheres were analyzed in terms of the respective contribution of gas-particle partitioning, cloud/fog processing of TMA(+) and DMA(+), bioaerosols, and sea-salt aerosols to the observed concentrations of the two ions over the seas.
引用
收藏
页码:3487 / 3498
页数:12
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