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還元性環境におけるチタンオーバーパックの水素吸収

Hydrogen absorption of titaniam for nuclear waste container in non-oxidizing condition

泊里 治夫*; 枡形 剛*; 下郡 一利*; 和田 隆太郎*; 本田 明; 谷口 直樹 

Tomari, Haruo*; not registered; Shimogori, Kazutoshi*; Wada, Ryutaro*; not registered; Taniguchi, Naoki

高レベル放射性廃棄物の地層処分においてオーバーパックの候補材料のひとつであるチタンの水素吸収挙動に関して、模擬地下水中でのベントナイト、印加電位、溶液のpH、陰分極試験時間の影響を検討した。水素吸収量の時間依存性を基に、水素吸収が放射物線則に従うと仮定して求めた水素吸収速度式から算出した1000年後の水素吸収量は、水素平衡電位近傍である-0.51Vvs.SHEでは約17ppmとなった。単位面積あたりの水素吸収量と平均の電解電流の対数との関係は直線性が得られ、水素吸収量の放射物則および今回行った程度の試験時間からの評価の妥当性が確認された。また、チタン中の水素量が約500ppmを超えた時点が脆化に対する臨界値と仮定した場合、チタンは地層処分環境下では1000年以上の寿命を有すると推察された。

Effects of bentonite clay, applied potential, pH, of solution and cathodic polarization time on hydrogen absorption into titanium, which is one of the candidate materials of overpack for high-level radioactive waste container, have been investigated in artificial underground water. Considering the result at various test time and assuming the hydrogen absorption is ruled by the paraboric law, the amount of hydrogen after 1000 years exposure calculated to about 17ppm, which will be absorbed at the applied potential of -0.51 vs. SHE corresponds to equilibrium potential of hydrogen. It seems the assumption of the parabolic law and the test period are proper, because the linear relations were obtained between the amount of absorbed hydrogen and the logarithm of the averaged cathodic current and between the slopes of the lines and a square root of the test time. Titanium seems to have a life over 1000 years in deep underground repository according to assumption that about 500ppm absorbed hydrogen is critical for hydrogen embrittlement of titanium.

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