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Artificial radionuclides recorded in recent sediments of Chinese lakes

https://repo.qst.go.jp/records/62922
https://repo.qst.go.jp/records/62922
f63ff345-1526-4269-b7b5-ad4d78c70ae7
Item type 会議発表用資料 / Presentation(1)
公開日 2008-12-17
タイトル
タイトル Artificial radionuclides recorded in recent sediments of Chinese lakes
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_c94f
資源タイプ conference object
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 Wu, Fengchang

× Wu, Fengchang

WEKO 621578

Wu, Fengchang

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Zheng, Jian

× Zheng, Jian

WEKO 621579

Zheng, Jian

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Liao, Haiqing

× Liao, Haiqing

WEKO 621580

Liao, Haiqing

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Yamada, Masatoshi

× Yamada, Masatoshi

WEKO 621581

Yamada, Masatoshi

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Wan, Guojiang

× Wan, Guojiang

WEKO 621582

Wan, Guojiang

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Wu Fengchang

× Wu Fengchang

WEKO 621583

en Wu Fengchang

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鄭 建

× 鄭 建

WEKO 621584

en 鄭 建

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Liao Haiqing

× Liao Haiqing

WEKO 621585

en Liao Haiqing

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山田 正俊

× 山田 正俊

WEKO 621586

en 山田 正俊

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抄録
内容記述タイプ Abstract
内容記述 Establishing accurate historical records of the distribution, inventory and source of artificial radionuclides in the environmental are important for environmental monitoring and radiological health protection due to its high toxicity, and useful for identification and risk assessment of possible future environmental inputs of radionuclides from nuclear weapons test and from the accidental release from the nuclear fuel reprocessing propocess and power plant reactor.
We applied a sector-field iCP-MS to study the recent sedimentation in ca. 20 lakes across China via measurements of both Pu isotopes, besides the conventional radiometric determination of 210Pb and 137Cs. The results show that the Pu activity profile was in agreement with the 137Cs profile in a sediment core of Lake Hongfeng. Inventories were 50.7 Bq/m2 foe 239+240Pu and 1586 Bq/m2 for 137Cs. the average 240Pu/239Pu atom ratio was 0.185 +/-0.009, indicating that Pu originated from global stratospheric fallout rather than from direct tropospheric or close-in fallout from the Chinese nuclear testing conducted in the 1970s. In the sediment core of lake Chenghai, the 240Pu/239Pu atom ratio ranged from 0.166 to 0.271 with a mean of 0.195 +/-0.021, which was slightly higher than that of global fallout. The 239+240Pu/137Cs activity ratios ranged from 0.0155 to 0.0411, with a mean of 0.0215, and the 239+240Pu inventory was 35.4 Bq/m2; both 239+240Pu/137Cs activity ratio and Pu inventory were close to those values of global fallout at 20-30 N. Three peaks were observed for both 137Cs and 239+240Pu activities in the examined sediment core; they most probably indicated the maximum deposition of global fallout between 1963 and 1964, the fallout from a series of Chinese nuclear tests during the 1970s, and the deposition of resuspended Pu-bearing particles from the Chernobyl accident. based on the isotopic compositions of Pu and isotopes and 137Cs distribuution, the sources of artificial radionuclides and teh potential application of Pu isotopes for sediment dating, and regional and global artificial effects were discussed.
会議概要(会議名, 開催地, 会期, 主催者等)
内容記述タイプ Other
内容記述 2008 Third Asia-Pacific Winter Conference on Plasma Spectrochemistry
発表年月日
日付 2008-11-21
日付タイプ Issued
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