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Dissolved radiocaesium in seawater off the coast of Fukushima during 2013-2015
https://repo.qst.go.jp/records/47692
https://repo.qst.go.jp/records/4769267b73ed9-7936-49ba-96f8-e0c9dcfcfe02
| Item type | 学術雑誌論文 / Journal Article(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2017-03-27 | |||||
| タイトル | ||||||
| タイトル | Dissolved radiocaesium in seawater off the coast of Fukushima during 2013-2015 | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| 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 | journal article | |||||
| アクセス権 | ||||||
| アクセス権 | metadata only access | |||||
| アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||
| 著者 |
Fukuda, Miho
× Fukuda, Miho× Aono, Tatsuo× Yamazaki, Shinnosuke× Nishikawa, Jun× Otosaka, Shigeyoshi× Ishimaru, Takashi× Kanda, Jota× 福田 美保× 青野 辰雄× 山崎 慎之介 |
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| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | To discuss the factors influencing radiocaesium distributions and its variation in the marine environment, dissolved radiocaesium was measured in seawater samples collected off the coast of Fukushima Prefecture during 2013-2015. The 137Cs activity concentrations in the surface-layer seawater at NPE2, NP0, NP2, NPE1, AN7, I01, E and A stations, which are located within about 10 km from the east coast of Japan, were higher than those at other stations. These high activity concentrations seem to be affected by several factors, including increased river input or contaminated water input from the Fukushima Dai-ichi Nuclear Power Station due to heavy rain events. | |||||
| 書誌情報 |
Journal of Radioanalytical and Nuclear Chemistry 巻 311, 号 2, p. 1479-1484, 発行日 2017-01 |
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| 出版者 | ||||||
| 出版者 | Springer Netherlands | |||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 0236-5731 | |||||
| DOI | ||||||
| 識別子タイプ | DOI | |||||
| 関連識別子 | 10.1007/s10967-016-5009-9 | |||||
| 関連サイト | ||||||
| 識別子タイプ | URI | |||||
| 関連識別子 | http://link.springer.com/article/10.1007/s10967-016-5009-9 | |||||
| 関連名称 | http://link.springer.com/article/10.1007/s10967-016-5009-9 | |||||
