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Transfer factor of radium-226 from soil to rice

https://repo.qst.go.jp/records/68485
https://repo.qst.go.jp/records/68485
5a41cff5-473b-4daf-9fd7-a6faf3efc264
アイテムタイプ 会議発表用資料 / Presentation(1)
公開日 2006-06-19
タイトル
タイトル Transfer factor of radium-226 from soil to rice
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 output
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 672300

Uchida, Shigeo

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Tagami, Keiko

× Tagami, Keiko

WEKO 672301

Tagami, Keiko

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Tabei, Ken

× Tabei, Ken

WEKO 672302

Tabei, Ken

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et.al

× et.al

WEKO 672303

et.al

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内田 滋夫

× 内田 滋夫

WEKO 672304

en 内田 滋夫

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田上 恵子

× 田上 恵子

WEKO 672305

en 田上 恵子

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田部井 健

× 田部井 健

WEKO 672306

en 田部井 健

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抄録
内容記述タイプ Abstract
内容記述 Transfer factor of radium-226 from soil to rice
\nS. Uchida1, K. Tagami1, K. Tabei2 and T. Fujikawa3
1 Office of Biospheric Assessment for Waste Disposal, National Institute of Radiological Sciences, Anagawa 4-9-1, Inage-ku, Chiba-shi, 263-8555, Japan
2 Tokyo Nuclear Services Co., Ltd., SA-Building 2F, Ueno 7-2-7, Taitou-ku, Tokyo, 110-0005 Japan
3 Kansai Environmental Engineering Center Co., Ltd., Azuchi-machi 1-3-5, Chu-o-ku, Osaka, 541-0052, Japan
\nAbstract
Radium-226 (Ra-226), an alpha emitter with a half-life of about 1600 y, is one of the important radionuclides for the assessment of radioactive waste disposal, because it is found in the uranium-238 decay series. Therefore it requires long-term management and understanding of Ra-226 behavior in the environment is of interest. Measurement of Ra-226 concentration in compartments of the environment gives us useful information for this purpose. In the environment, radium occurs naturally and distributed widely in environmental materials, such as rock, soil, water and plants, however, usually Ra-226 concentration is very low. It is difficult to measure Ra-226 without chemical separation and concentration from sample matrices, especially for plant samples. Thus, soil-to plant transfer factor (TF) data are limited for mathematical models for a precise long-term radiological assessment.
In this study, we determine the concentrations of Ra-226 in rice grains and associated paddy soils using radiation counting methods. We focused on rice and wheat, because the consumption of cereals is very high in Japan and other Asian countries. The rice samples and the paddy soils were collected from 11 locations throughout Japan. For soil samples, they were air-dried and sieved with a 2-mm sieve. About 60-g of each pretreated soil sample was charged and sealed into a plastic vessel. The sample was kept in a room temperature for more than 30 days to reach an equilibrium condition with its progeny nuclides. Then, the concentration of Pb-214 was determined by a Ge detector system. For the rice samples, they were incinerated at 450?C for 24 h after they husked. Then, a chemical separation was carried out using about 15 g of the incinerated sample. It was recommended to use about 5 g of incinerated rice in a standard method, however, to obtain lower level of detection limit (D.L.), the sample amount was increased by three times in the present study. After the chemical separation, Ra-226 concentration was determined by a liquid scintillation counter system. The chemical yield of Ra was obtained directly but barium (Ba) was used as a yield tracer in the samples because they have similar chemical behaviors. To check the accuracy of the method, we used IAEA-315 (marine sediment) and IAEA-368 (Pacific ocean sediment); no standard reference material is available for plant samples.
The recoveries of Ba for Ra were more than 97% for all the samples. Detection limit was lowered since a 15-g of sample was applied; that is, the D.L. was about 0.7 Bq/kg-dry, while it was about 2 Bq/kg when a 5-g of soil sample, a typical weight for the standard method, was used. The concentrations of Ra-226 in paddy soil samples ranged from 20 to 65 Bq/kg-dry soil, and those in the brown rice samples ranged from 8 to 65 mBq/kg-dry except for two samples (<D.L.). Using the data, TFs were calculated and the average TF of Ra-226 from the paddy soil to the rice (brown rice) was 6.8E-04. The value was close to TFs for maize reported in technical report series No. 364, IAEA.
In the presentation, we will report the details of the chemical separation conditions and radiation measurement conditions as well as Ra-226 values in soil and rice samples determined by the developed method.
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 Waste Management 2005
発表年月日
日付 2005-03-03
日付タイプ Issued
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