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Transfer factors of radionuclides from soil to rice and wheat collected in Japan

https://repo.qst.go.jp/records/53669
https://repo.qst.go.jp/records/53669
34194718-1bb6-4dba-b6ed-ada6093755c7
Item type 会議発表論文 / Conference Paper(1)
公開日 2006-06-05
タイトル
タイトル Transfer factors of radionuclides from soil to rice and wheat collected in Japan
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_5794
資源タイプ conference paper
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 Uchida, Shigeo

× Uchida, Shigeo

WEKO 547788

Uchida, Shigeo

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Tagami, Keiko

× Tagami, Keiko

WEKO 547789

Tagami, Keiko

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Hirai, Ikuko

× Hirai, Ikuko

WEKO 547790

Hirai, Ikuko

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et.al

× et.al

WEKO 547791

et.al

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内田 滋夫

× 内田 滋夫

WEKO 547792

en 内田 滋夫

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田上 恵子

× 田上 恵子

WEKO 547793

en 田上 恵子

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平井 育子

× 平井 育子

WEKO 547794

en 平井 育子

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内容記述タイプ Abstract
内容記述 Obtaining local soil-to-crop transfer factor (TF) is important because climates, soil types and vegetations influence on the factor. In this study, analyses of stable isotopes and natural radioisotopes in rice and wheat grains and the associated soils collected throughout Japan were carried out in order to obtain TF under equilibrium conditions. The studied samples had been collected for the measurement of global fallout 137Cs and 90Sr at National Institute of Agro-Environmental Sciences. Inductively coupled plasma mass spectrometry and inductively coupled plasma optical emission spectrometry were used to measure about 30 elements, including Cs, Sr, Th and U. The geometric-mean-TFs of Cs, Sr, Th and U for polished rice collected in Akita, Japan, were 0.0024, 0.0037, 0.0001 and 0.000053, respectively. The results indicated that TF-Cs was usually lower than TF-137Cs (geometric mean=0.0033). Possibly, the physico-chemical forms of stable Cs differed from those of global fallout 137Cs in the soil samples, that is, a part of the stable Cs was strongly fixed in the soil particles, while 137Cs was more mobile in the soil. However, the difference of TF-Cs and -137Cs was small, thus, the TF-Cs can be used for long-term transfer of 137Cs in the environment. The methodology would be applied to the other elements, though physico-chemical forms of natural and non-natural isotopes should be clarified.
書誌情報 Proceedings of International Congress of the International Radiation Protection Association

巻 11, p. 6d19, 発行日 2004-05
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