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インド洋および南極海における浮遊粒子状物質の化学組成に関する研究
https://kindai.repo.nii.ac.jp/records/18448
https://kindai.repo.nii.ac.jp/records/1844843ffa7de-5bf1-46f7-82b4-74ba77ca5dc2
名前 / ファイル | ライセンス | アクション |
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AN10074306-20160228-0001.pdf (489.5 kB)
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Item type | ☆紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2017-06-13 | |||||
タイトル | ||||||
タイトル | インド洋および南極海における浮遊粒子状物質の化学組成に関する研究 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Studies on the chemical composition of suspended particulate matter in the Indian and the Antarctic Ocean | |||||
著者 |
中口, 譲
× 中口, 譲× 廣田, 晶子 |
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言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題 | suspended particle, chemical composition, the Indian Ocean, the Antarctic Ocean, individual particle analysis | |||||
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 | |||||
著者(英) | ||||||
en | ||||||
Nakaguchi,Yuzuru | ||||||
著者(英) | ||||||
en | ||||||
Hirota,Akiko | ||||||
著者 所属 | ||||||
近畿大学 | ||||||
著者 所属 | ||||||
近畿大学 | ||||||
著者所属(翻訳) | ||||||
School of Science and Engineering, Kinki University: Research Institute for Science and Technology, Kinki University: Interdisciplinary Graduate School of Science and Engineering, Kinki University | ||||||
著者所属(翻訳) | ||||||
School of Science and Engineering, Kinki University | ||||||
版 | ||||||
出版タイプ | NA | |||||
出版タイプResource | http://purl.org/coar/version/c_be7fb7dd8ff6fe43 | |||||
出版者 名前 | ||||||
出版者 | 近畿大学理工学総合研究所 | |||||
書誌情報 |
理工学総合研究所研究報告 en : Annual reports by Research Institute for Science and Technology 号 28, p. 1-11, 発行日 2016-02-28 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 09162054 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | [Abstract] The origin of particulate matter which collected from the Indian Ocean and the Antarctic Ocean was clarified by individual particle analysis. Iron-rich particle which carried from land was observed at the surface in all sampling stations. Aluminum-dominant and Al-Si particles were observed at ER-5, 8 and 10 in the Indian Ocean sampling stations. These results confirmed that these particles were land origin such as aluminosilicate. A lot of silica dominant particles were observed at ER-14 in the Antarctic Ocean station. The SEM image of these particulate matter suggested that these particles were originated from diatom. The number of biogenic particles which exist at the surface has decreased with increase of depth. | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf |