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Liu, J.; 土津田 雄馬; 北垣 徹; 青柳 登; Mei, H.; 高野 公秀; 香西 直文
Journal of Nuclear Science and Technology, 60(8), p.1002 - 1012, 2023/08
被引用回数:1 パーセンタイル:18.87(Nuclear Science & Technology)This study aims to reveal the potential bacterial alteration of nuclear fuel debris. A melt simulant composed of U
Zr
O
and Fe(0), and three powder simulants (UO
, Fe(0), and their mixed powder) were prepared and exposed to Bacillus subtilis in a Fe-deficient medium under aerobic conditions. B. subtilis could not dissolve Zr from the melt simulant but enhanced the dissolution of U and Fe, although the change of the melt simulant was too small to evaluate. Experiments using powder simulants were performed to investigate the bacterial influence in detail. B. subtilis enhanced the dissolution of U from the UO
powder and Fe from the Fe(0) powder, although the dissolution of U was low. Most aqueous U species were probably U(VI), while the U that remained as a solid phase was mostly U(IV). The Fe(0) powder was oxidized by this bacterium, transforming it into an aqueous and solid Fe species. The stable species consisted of amorphous nano-sized particles. A fraction of the dissolved Fe was adsorbed or precipitated onto the UO
particles and remained undissolved. These results strongly suggest that bacteria can degrade nuclear fuel debris, although this study did not elucidate the mechanism of oxidative dissolution.
Martin, A. J.*; 亀井 玄人; 塩月 正雄; 黒田 茂樹*
Proceedings of International Waste Management Symposium 2007 (WM '07) (CD-ROM), 12 Pages, 2007/03
日本の電気事業連合会と日本原子力研究開発機構は、高レベル廃棄物処分の研究成果を基盤としつつ、TRU廃棄物の安全な処分について、関係機関と研究開発を行ってきた。この研究協力(プロジェクトTRU-2)は、日本のTRU廃棄物処分の研究開発に一つの進展をもたらした。本論文は、このプロジェクトの概要を記すもので、鍵となる成果と幾つかの独創的方法論が示されている。
SiO
determined by high
in situ X-ray diffractometry桂 智男*; 山田 均*; 新名 亨*; 久保 敦*; 小野 重明*; 神崎 正美*; 米田 明*; Walter, M. J.*; 伊藤 英司*; 浦川 啓*; et al.
Physics of the Earth and Planetary Interiors, 136(1-2), p.11 - 24, 2003/04
被引用回数:186 パーセンタイル:93.73(Geochemistry & Geophysics)Mg
SiO
のポストスピネル相転移境界をKawai型高圧装置と放射光を組合せた高温高圧下その場X線回折実験により再決定した。その結果、1550
2100Kにおける相境界は、約22GPaであり、地球内部660Km不連続が想定されている圧力より1
1.5GPa低かった。