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  1. 原著論文

Reprint of "Vertical migration of radio-caesium derived from the Fukushima Dai-ichi Nuclear Power Plant accident in undisturbed soils of grassland and forest"

https://repo.qst.go.jp/records/48773
https://repo.qst.go.jp/records/48773
51738f7e-5b1f-4086-aea3-8742df062055
Item type 学術雑誌論文 / Journal Article(1)
公開日 2018-04-23
タイトル
タイトル Reprint of "Vertical migration of radio-caesium derived from the Fukushima Dai-ichi Nuclear Power Plant accident in undisturbed soils of grassland and forest"
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 S.Mishra

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WEKO 491023

S.Mishra

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S.K.Sahoo

× S.K.Sahoo

WEKO 491024

S.K.Sahoo

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P.Bossew

× P.Bossew

WEKO 491025

P.Bossew

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A.Sorimachi

× A.Sorimachi

WEKO 491026

A.Sorimachi

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S.Tokonami

× S.Tokonami

WEKO 491027

S.Tokonami

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サフー サラタ クマール

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WEKO 491028

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抄録
内容記述タイプ Abstract
内容記述 The vertical distribution of radio-caesium (137Cs and 134Cs) in undisturbed soil profiles of grassland and forest soils, derived from the Fukushima-Daiichi Nuclear Power Plant (FDNPP) accident that occurred on 11 March 2011, was studied. Surface soil and depth profile soil samples were collected from six locations within the 20 km zone of FDNPP, during November 2012 and June 2013. The activity ratio for 137Cs and 134Cs was found to be almost constant about 1 within the soil profiles as well as in the surface soil, indicative of FDNPP accident origin. From soil depth profile distribution of Cs activity, it is observed that Cs is strongly bound to soil materials, which slows Cs migration. N90% of the activity was found to be retainedwithin the upper 5 cmlayer. Retardation of Cs movement has been quantified by measuring sorption of Cs in soil in terms of distribution coefficient (Kd) using the laboratory batch method. Faster migration has been observed in case of forest land soil compared to grassland soil. The empirical migration velocity of Cs radio isotope was estimated fromthe depth profile Cs concentration
and found to vary from 1.1 to 1.7 and 0.85 to 3.5 cm y−1 in grassland and forest soil, respectively. The residential half life for Cs isotopes was found to be 1.03–7.75 y and 1.18–4.67 y for grassland and forest land respectively using a compartmental model. In addition to the empirical analysis of the profiles, analytical models
were fitted to the data which may help elucidate the physical nature of the transport of trace elements.
書誌情報 Journal of Geochemical Exploration

巻 184, p. 271-295, 発行日 2018-03
出版者
出版者 Elsevier
ISSN
収録物識別子タイプ ISSN
収録物識別子 0375-6742
DOI
識別子タイプ DOI
関連識別子 10.1016/j.gexplo.2016.07.023
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