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大気中の元素状炭素粒子の粒径分布
https://doi.org/10.14945/00000389
https://doi.org/10.14945/00000389187da666-316f-4223-8d6e-521138bacf91
名前 / ファイル | ライセンス | アクション |
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KJ00000102490.pdf (970.9 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2008-01-25 | |||||||
タイトル | ||||||||
タイトル | 大気中の元素状炭素粒子の粒径分布 | |||||||
言語 | ||||||||
言語 | jpn | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | elemental carbon | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | size distribution | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | Andersen-type high volume air sampler | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | fog | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | rain and daily variation | |||||||
資源タイプ | ||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
資源タイプ | departmental bulletin paper | |||||||
ID登録 | ||||||||
ID登録 | 10.14945/00000389 | |||||||
ID登録タイプ | JaLC | |||||||
タイトル(別言語) | ||||||||
その他のタイトル | Size distribution of elemental carbon in the atmosphere | |||||||
著者 |
中島, 賢邦
× 中島, 賢邦× 太田良, 和弘× 鈴木, 款
WEKO
334
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書誌情報 |
静岡大学地球科学研究報告 巻 29, p. 45-52, 発行日 2002-07 |
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出版者 | ||||||||
出版者 | 静岡大学地球科学教室 | |||||||
NDC | ||||||||
主題Scheme | NDC | |||||||
主題 | 451 | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | Elemental carbon (EC) is produced by incomplete combustion of fossil fuel and vegetation. In this study, we determined size distribution of EC in the atmosphere. Observation was conducted at Shizuoka Univ., Mizugatsuka Park (the Mt. Fuji), the Mt. Norikura and Shigaraki. Aerosol samples were collected with an Andersen-type high volume air sampler as for the size-range of <1.1 μm, 1.1-2.0 μm, 2.0-3.3 μm, 3.3 - 7.0 μm and >7.0 μm in diameter, respectively. Concentration of EC in <1.1 μm-fraction was the higher than the other fraction on sunny days, suggesting a significant effect of EC in <1.1 μm-fraction on the level of total EC. Concentration of total EC on foggy days was as same as that of total EC on sunny days at the Mt. Norikura, while concentration of EC in >3.3 μm-fraction on foggy days was higher than that on sunny days. This result implies that EC acts as nuclei of cloud condensation, and its size becomes larger in the clouds compared to the original size. Concentration of EC in <1.1 μm-fraction was remarkably lower on rainy days than those on sunny days, while the difference in the other fractions was relatively small between rainy and sunny days, suggesting EC in <1.1 μm-fraction is dominantly taken into rainwater. Variation of EC in the total and <1.1 μm-fraction was markedly small (10 - 13%) at Midzugatsuka compared to that in the other sites, suggesting that some process would work to keep the level of EC as constant. | |||||||
ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 03886298 | |||||||
NII論文ID | ||||||||
関連タイプ | isIdenticalTo | |||||||
識別子タイプ | NAID | |||||||
関連識別子 | 110000413414 | |||||||
NII書誌ID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AN00103190 | |||||||
フォーマット | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | application/pdf | |||||||
著者版フラグ | ||||||||
出版タイプ | VoR | |||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |