@article{oai:nipr.repo.nii.ac.jp:00003612,
 author = {ニシカワ, マサタカ and ミゾグチ, ツグオ and カナモリ, サトル and カナモリ, ノブコ and アオキ, シュンジ and カワグチ, サダオ and NISHIKAWA, Masataka and MIZOGUCHI, Tsuguo and KANAMORI, Satoru and KANAMORI, Nobuko and AOKI, Shuhji and KAWAGUCHI, Sadao},
 journal = {Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology},
 month = {Jan},
 note = {P(論文), Fifty-eight samples were collected over the Antarctic Sea between December 3 and 31 in 1987. The sampling was carried out on board the research vessel "SHIRASE" by a medium volume sampler, which can be automatically operated every 12h at the sampling rate of 150l/min. The samples were analyzed for Na, Mg, Al, K, Ca, V, Mn, Fe, Ni, Cu, Zn, Sr, Mo, Ag, Cd, Ba and Pb for ICP-AES, and for NH_4^+, Cl^-, NO_3^- and SO_4^<2-> by ion chromatography. It is considered that aerosol derived from the crust has a concentration on the order of 10ng/m^3 over the Antarctic Sea. This estimated value is about 1/10 that over the East China Sea near Japan. The excess sulfate aerosol has a concentration on the order of 100ng/m^3 over that sea. Thus, the excess sulfate aerosol was defined as follows : (excess SO_4=SO_4-0.25×Na)_<in weight> Because of the mole ratio between excess SO_4^<2-> and Na, which was comparable to the amount of Cl loss on a mole basis, it must be present the combination as Na_2SO_4. It is considered that Cl loss is due to the reaction of sea salt aerosol with sulfate aerosol even over the Antarctic Sea.},
 title = {CHEMICAL COMPONENTS OF MARINE AEROSOL OVER THE ANTARCTIC SEA},
 volume = {3},
 year = {1990}
}