Atmospheric particle dry deposition of major ions to the South Atlantic coastal area observed at Baia de Todos os Santos, Brazil

被引:14
|
作者
Mkoma, Stelyus L. [1 ,2 ,3 ]
da Rocha, Gisele O. [1 ,2 ]
Domingos, Jose S. S. [2 ]
Santos, Joao V. S. [1 ,4 ]
Cardoso, Manuela P. [2 ]
da Silva, Rogerio L. [2 ]
de Andrade, Jailson B. [2 ]
机构
[1] Inst Nacl Ciencia & Tecnol Energia & Ambiente INC, BR-40110040 Salvador, BA, Brazil
[2] Univ Fed Bahia UFBA, Inst Quim, BR-40170290 Salvador, BA, Brazil
[3] SUA, Fac Sci, Dept Phys Sci, Morogoro, Tanzania
[4] Inst Fed Educ Ciencia & Tecnol Baiano, BR-45995000 Teixeira De Freitas, BA, Brazil
来源
关键词
particle dry deposition; PM; major ions; tropical atmosphere; Baia de Todos os Santos bay; Brazil; POLYCYCLIC AROMATIC-HYDROCARBONS; WEIGHT DICARBOXYLIC-ACIDS; SIZE DISTRIBUTION; TRACE-METALS; SEASONAL-VARIATION; SITES; AEROSOL; REGION; URBAN; FINE;
D O I
10.1590/0001-3765201420130234
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The coastal atmosphere adjacent to large urban areas can be strongly affected by the emission of air pollutants, among them, major ions species. In this study, the chemical composition and sources of carboxylates and other water-soluble ions in fine and coarse aerosols as well as estimates of particle dry deposition fluxes were studied at a tropical coastal site affected by an urban environment. The mean concentrations of the total carboxylates were 78 ng m(-3) in fine fraction and 81 ng m(-3) in coarse fraction of particulate matter ( PM). The corresponding values for the total inorganic ions were 2143 ng m-3 and 4880 ng m(-3) respectively. Main sources for fine particles were: (i) photochemical formation of carboxylic acids in vapor phase and a posterior gas-to-particle conversion onto sea salt particles; (ii) emissions from anthropic sources with long range transportation processes; and (iii) the interchanging of volatile species among atmospheric phases. In turn, for coarse particles, the predominant sources were: ( i) gas-phase species and ab/adsorbed onto preexisting particles afterwards; ( ii) primary emission of coarse particles from anthropogenic sources; and ( iii) sea salt spray and/or soil resuspension. Finally, particle dry deposition was a very important mechanism representing air-to-sea fluxes of major species.
引用
收藏
页码:37 / 55
页数:19
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