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Contribution of bacteria on the insoluble technetium formation in paddy soil surface water

https://repo.qst.go.jp/records/68113
https://repo.qst.go.jp/records/68113
be457dad-abcb-4919-9256-d3eaa677b6a9
Item type 会議発表用資料 / Presentation(1)
公開日 2005-07-11
タイトル
タイトル Contribution of bacteria on the insoluble technetium formation in paddy soil surface water
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 668874

Ishii, Nobuyoshi

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Tagami, Keiko

× Tagami, Keiko

WEKO 668875

Tagami, Keiko

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Uchida, Shigeo

× Uchida, Shigeo

WEKO 668876

Uchida, Shigeo

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石井 伸昌

× 石井 伸昌

WEKO 668877

en 石井 伸昌

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田上 恵子

× 田上 恵子

WEKO 668878

en 田上 恵子

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内田 滋夫

× 内田 滋夫

WEKO 668879

en 内田 滋夫

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内容記述タイプ Abstract
内容記述 Tecchnetium-99 (99Tc) is a fission product of 235U and 239Pu with a relatively high yield of about 6%. The half-life of this radionuclide is 2.1 * 10^5 years, implying its presence in the environment for many generations. The main sources of 99Tc in the environment are nuclear weapons testing and nuclear fuel reprocessing plants.
In aerobic conditions, Tc is present as pertechnetate (TcO4-), which is both highly soluble and mobile in the environment. It acts as a sulfate analog and assimilation of TcO4- by plants raises concern about the transfer of 99Tc to human though agricultural plants. We previously reported that Tc in agricultural soil surface water would transform from soluble TcO4- to insoluble form (> 0.2 um in size). It is difficult for the plant to take in the insoluble Tc in this size.
The formation of insoluble Tc in the soil surface waters seems to be caused by microorganisms. In this study we describe kinds of microbes contribute to the insoluble Tc.
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 30th Annual Meeting
発表年月日
日付 2004-03-04
日付タイプ Issued
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