Characterization of atmospheric air pollutants at two sites in northern Kyushu, Japan - chemical form, and chemical reaction

Citation
T. Shimohara et al., Characterization of atmospheric air pollutants at two sites in northern Kyushu, Japan - chemical form, and chemical reaction, ATMOS ENVIR, 35(4), 2001, pp. 667-681
Citations number
19
Categorie Soggetti
Environment/Ecology,"Earth Sciences
Journal title
ATMOSPHERIC ENVIRONMENT
ISSN journal
13522310 → ACNP
Volume
35
Issue
4
Year of publication
2001
Pages
667 - 681
Database
ISI
SICI code
1352-2310(2001)35:4<667:COAAPA>2.0.ZU;2-L
Abstract
Airborne gaseous and particulate matter in winter was measured over for 37 days in January and December 1997 at ? sampling sites in northern Kyushu, J apan. One sampling site, Goto Island tan isolated island in the East China Seal. was about 200 km southwest of the other sampling site, Dazaifu city. In winter, acidic sulfates generated over the East Asian continent were tra nsported to northwest Kyushu, to places such as Goto Island and the inland Kyushu areal and high sulfate concentrations were observed at the 2 samplin g sites when strong NW winds blew, Acidity around Golo was mainly influence d by particulate NH,HSOS. The concentrations of NH3 at Goto Island were low er than at Dazaifu city. The difference in NH3, levels at the 2 sampling si tes plays an important role in the chemical forms and sizes of the particul ate matter. Nitrates at Goto Island were mostly present as NaNO3 and Ca(NO3 )(2) in coarse-size particles. During the process of long-range transport o f air pollutants From the Asian continent to Goto, gaseous HNO3 was produce d by a photochemical reactions of nitrogen oxides in the atmosphere, and pa rticulate NaNO3 and gaseous HCl were formed by a chlorine-loss reaction bet ween NaCl and gaseous HNO3. When strong NW winds blew, acidic sulfates toge ther with some of the NaNO3 and/or Ca(NO3)(2) and some of gaseous HCl and H NO3, which exist in the sea to the west of Kyushu and Goto Island, were tra nsported to inland Kyushu such as Dazaifu city. During the process of trans port, most of the acidic sulfates and acidic gases were mixed with regional air pollutants such as chlorides and nitrates existing around Dazaifu city , and neutralized forming (NH4)(2) SO4, NH4Cl and NH4NO3 in an environment of excess NH3. Therefore, the main chemical forms of NO; at Dazaifu city va ried day-by-day from fine-sized NH4NO3 to coarse-sized NaNO3 and/or Ca(NO3) (2). The appearance of NO3- in coarse-size particles at Dazaifu city was du e to the transport of NO3- from around the sea to the west of Kyushu. (C) 2 001 Published by Elsevier Science Ltd.