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  1. 原著論文

Pu and Cs-137 in Yangtze River estuary sediments: distribution and source identification

https://repo.qst.go.jp/records/46026
https://repo.qst.go.jp/records/46026
fe500ae0-cf03-427a-ac88-0439fa0824d4
Item type 学術雑誌論文 / Journal Article(1)
公開日 2011-04-04
タイトル
タイトル Pu and Cs-137 in Yangtze River estuary sediments: distribution and source identification
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 Liu, Zhiyong

× Liu, Zhiyong

WEKO 458054

Liu, Zhiyong

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Zheng, Jian

× Zheng, Jian

WEKO 458055

Zheng, Jian

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Pan, Shaoming

× Pan, Shaoming

WEKO 458056

Pan, Shaoming

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Dong, Wei

× Dong, Wei

WEKO 458057

Dong, Wei

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Yamada, Masatoshi

× Yamada, Masatoshi

WEKO 458058

Yamada, Masatoshi

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Aono, Tatsuo

× Aono, Tatsuo

WEKO 458059

Aono, Tatsuo

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Guo, Qiuju

× Guo, Qiuju

WEKO 458060

Guo, Qiuju

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劉 志勇

× 劉 志勇

WEKO 458061

en 劉 志勇

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鄭 建

× 鄭 建

WEKO 458062

en 鄭 建

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董 微

× 董 微

WEKO 458063

en 董 微

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山田 正俊

× 山田 正俊

WEKO 458064

en 山田 正俊

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青野 辰雄

× 青野 辰雄

WEKO 458065

en 青野 辰雄

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抄録
内容記述タイプ Abstract
内容記述 Pu isotopes and 137Cs were analyzed using sector field ICP-MS and gama spectrometry, respectively, in surface sediment and core sediment samples from the Yangtze River estuary. 239+240Pu activity, 240Pu/239Pu atom ratios (higher than 0.18) shows a generally increasing trend from land to sea and from north to south in the estuary. This spatial distribution pattern indicates that the Pacific Proving Grounds (PPG) source Pu transported by ocean currents was intensively scavenged into the suspended sediment under favorable conditions, and mixed with riverine sediment as the water circulated in the estuary. This process is the main control for the distribution of Pu in the estuary. Moreover, Pu is also an important indicator for monitoring the changes of environmental radioactivity in the estuary as the river basin is currently the site of extensive human activities and the sea level is rising because of global climate changes. For core sediment samples the maximum peak of 239+240Pu activity was observed at a depth of 172 cm. The sedimentation rate was estimated on the basis of the Pu maximum deposition peak in 1963-1964 to be 4.1cm/a. The contributions of the PPG close-in fallout Pu (44%) and the riverine Pu (45%) in Yangtze River estuary sediments are equally important for the total Pu deposition in the estuary, which challenges the current hypothesis that the riverine Pu input was the major source of Pu budget in this area.
書誌情報 Environmental Science & Technology

巻 45, 号 5, p. 1805-1811, 発行日 2010-03
ISSN
収録物識別子タイプ ISSN
収録物識別子 0013-936X
関連サイト
識別子タイプ URI
関連識別子 http://pubs.acs.org
関連名称 http://pubs.acs.org
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