@article{oai:nipr.repo.nii.ac.jp:00009573,
 author = {原, 圭一郎 and 長田, 和雄 and 西田, 千春 and 矢吹, 正教 and 林, 政彦 and 山内, 恭 and 和田, 誠 and 塩原, 匡貴 and Hara, Keiichiro and Osada, Kazuo and Nishita-Hara, Chiharu and Yabuki, Masanori and Hayashi, Masahiko and Yamanouchi, Takashi and Wada, Makoto and Shiobara, Masataka},
 issue = {特集号},
 journal = {南極資料, Antarctic Record},
 month = {Dec},
 note = {P(論文), 第46-47次日本南極地域観測隊で,超微小粒子の粒径分布とその揮発特性の連続観測を実施した.夏季には超微小粒子のほとんどは揮発性粒子で,硫酸,メタンスルホン酸,硫酸塩で構成されていた.夏には超微小粒子域の非揮発性粒子の割合は20% だったが,冬季には90% を超すこともあった.冬季の超微小粒子のほとんどは海塩粒子であり,海氷上で組成分別をした海塩粒子も含まれていた.南極大陸内陸部上空から昭和基地(沿岸部)に空気塊が輸送される時には,冬季にも揮発性粒子の割合が減少していた., The Size distribution and volatility of ultrafine aerosol particles were measured at Syowa Station during the 46-47 Japanese Antarctic Research Expeditions. During the summer, most of the ultrafine particles were volatile particles, which were composed of H_2SO_4, CH_3SO_3H and sulfates bi-sulfates. The abundance of non-volatile particles was ～ 20% during the summer, increasing to>90% in winter-spring. Non-volatile particles in winter were dominantly sea-salt particles. Some ultrafine sea-salt particles might be released from sea-ice. When air mass was transported from the free troposphere over the Antarctic continent, the abundance of non-volatile particles dropped to<30% even in winter.},
 pages = {541--553},
 title = {南極対流圏中の超微小粒子の揮発特性とその季節変化},
 volume = {54},
 year = {2010},
 yomi = {ハラ, ケイイチロウ and オサダ, カズオ and ニシダ, チハル and ヤブキ, マサノリ and ハヤシ, マサヒコ and ヤマノウチ, タカシ and ワダ, マコト and シオバラ, マサタカ}
}