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花崗閃緑岩,凝灰質砂岩試験片に対するヨウ素,スズの分配係数

Distribution coefficients of iodine and tin on granodiorite and tuffaceous sandstone specimens

邉見 光; 山口 徹治; 飯田 芳久

Hemmi, Ko; Yamaguchi, Tetsuji; Iida, Yoshihisa

ヨウ素とスズは、地層処分の安全評価上重要な元素である。ヨウ素の分配係数として有意な値を期待できるのかどうかを見極めるために中性付近にてNaNO$$_{3}$$濃度を0-0.5mol dm$$^{-3}$$の範囲で変化させて収着試験を実施した。誤差を評価して分配係数を求めた結果、凝灰質砂岩については、NaNO$$_{3}$$濃度0.5mol dm$$^{-3}$$の条件を除きゼロではない有意な値を持ち、花崗閃緑岩については、NaNO$$_{3}$$濃度0.5mol dm$$^{-3}$$以上の条件では有意な値を持つことが示された、スズについては、加水分解により生成する陰イオン種の増加とともに分配係数が著しく低下する可能性が考えられるため、高pH条件にて収着試験を実施した。花崗閃緑岩の分配係数はpH10.4で9.79$$times$$10$$^{-2}$$m$$^{3}$$kg$$^{-1}$$となり、pH12.4で2.46$$times$$10$$^{-3}$$m$$^{3}$$kg$$^{-1}$$の値となった。凝灰質砂岩については、pH12.4付近で花崗閃緑岩より1桁程度高い分配係数(約2$$times$$10$$^{-2}$$m$$^{3}$$kg$$^{-1}$$)が得られた。

Iodine and tin are important elements in performance assessment of geological disposal of radioactive wastes. Sorption experiments of iodine were carried out under varying nitrate concentration with a range of 0 to 5 mol dm$$^{-3}$$ at neutral pH range in order to determine the distribution coefficient of iodine was zero or non-zero value. The experimental results with estimated statistical errors showed non-zero values for tuffaceous sandstone except for NaNO$$_{3}$$ concentration 0.5 mol dm$$^{-3}$$. Non-zero values were also obtained under NaNO$$_{3}$$ concentrations higher than 0.5 mol dm$$^{-3}$$ for granodiorite. Sorption experiments of tin were carried out at high pH range in order to check whether the distribution coefficient of tin decreases significantly with pH as a result of formation of anionic hydrolysis species of tin. The distribution coefficients of tin on granodiorite decreased from 9.79$$times$$10$$^{-2}$$ m$$^{3}$$ kg$$^{-1}$$ at pH10.4 to 2.46$$times$$10$$^{-3}$$ m$$^{3}$$ kg$$^{-1}$$ at pH12.4. The distribution coefficient of tin on tuffaceous sandstone was about one order of magnitude higher (about 2$$times$$10$$^{-2}$$ m$$^{3}$$ kg$$^{-1}$$) than that of granodiorite at pH around 12.4.

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