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Determination of carbon species formed by decomposition of acetate in Japanese paddy soil

https://repo.qst.go.jp/records/70466
https://repo.qst.go.jp/records/70466
4e5c546e-42c1-461e-8daa-4d85321c964f
Item type 会議発表用資料 / Presentation(1)
公開日 2011-06-29
タイトル
タイトル Determination of carbon species formed by decomposition of acetate in Japanese paddy soil
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 Ishii, Nobuyoshi

× Ishii, Nobuyoshi

WEKO 691991

Ishii, Nobuyoshi

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Koiso, Hiroyuki

× Koiso, Hiroyuki

WEKO 691992

Koiso, Hiroyuki

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Uchida, Shigeo

× Uchida, Shigeo

WEKO 691993

Uchida, Shigeo

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石井 伸昌

× 石井 伸昌

WEKO 691994

en 石井 伸昌

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小礒 寛之

× 小礒 寛之

WEKO 691995

en 小礒 寛之

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内田 滋夫

× 内田 滋夫

WEKO 691996

en 内田 滋夫

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抄録
内容記述タイプ Abstract
内容記述 Transuranic (TRU) waste containing radionuclides is generated during the operation and dismantling of reprocessing facilities and mixed oxide (MOX) fuel fabrication facilities. In Japan, TRU waste for geological disposal is grouped into four gropes in accordance with physical properties and the concentration of radioactive materials. Group 2 waste among four groups of TRU waste includes hull and end piece wastes, which are comprised of the debris and residue from the shearing and dissolution of the spent fuel assemblies. The key nuclide in a geological repository for Group 2 waste is C-14, and leaching of organic C-14 compounds from simulated hull wastes has been reported. Because organic C-14 is long-lived and has very little sorption properties, the possible migration of C-14 from a TRU repository site to the biosphere through groundwater presents some concern. Therefore, it is necessary to understand the behavior of C-14 in the human habitation sphere on the assumption the C-14 derived from TRU wastes.
\nRice paddy field is one of important places to assess the behavior of C-14 because rice has long been a staple food in the Japanese diet and people may be expose to C-14 through rice intake. Radioactive tracer experiments with [1,2-C-14] sodium acetate showed that more than 60% of the spiked C-14 was released from flooded paddy soil samples into the air as gas forms. Rice plants may assimilate the released C-14 depending on chemical species. The chemical species of the released C-14, however, have not been identified yet. This paper will show the main chemical species of C-14 in gas phase, which was formed by decomposition of acetate by microorganisms in the paddy soil.
\nThis work has been partially supported by the Agency for Natural Resources and Energy, the Ministry of Economy, Trade and Industry (METI) Japan.
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 International Conference on Radioecology and Environmental Radioactivity
発表年月日
日付 2011-06-24
日付タイプ Issued
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