CEA, DEN, DEC, SPUA, LMPC, F-13108 Saint-Paul-lez Durance, France.
Inorg Chem. 2013 Mar 4;52(5):2519-25. doi: 10.1021/ic302457m. Epub 2013 Feb 14.
Incorporating minor actinides (MAs = Am, Np, Cm) in UO2 fertile blankets is a viable option to recycle them. Despite this applied interest, phase equilibria between uranium and MAs still need to be thoroughly investigated, especially at elevated temperatures. In particular, few reports on the U-Np-O system are available. In the present work, we provide for the first time in situ high-temperature X-ray diffraction results obtained during the oxidation of (U1-yNpy)O2 uranium-neptunium mixed oxides up to 1373 K and discuss subsequent phase transformations. We show that (i) neptunium stabilizes the UO2-type fluorite structure at high temperature and that (ii) the U3O8-type orthorhombic structure is observed in a wide range of compositions. We clearly demonstrate the incorporation of neptunium in this phase, which was a controversial question in previous studies up to now. We believe it is the particular stability of the tetravalent state of neptunium that is responsible for the observed phase relationships.
将少量锕系元素(MA=镅、镎、锔)纳入二氧化铀增殖层是回收它们的可行方案。尽管人们对此应用很感兴趣,但铀与 MA 之间的相平衡仍需要进行彻底研究,尤其是在高温下。特别是,关于 U-Np-O 体系的报道很少。在本工作中,我们首次提供了在 1373 K 下氧化(U1-yNpy)O2 铀-镎混合氧化物过程中获得的原位高温 X 射线衍射结果,并讨论了随后的相变。我们表明:(i)在高温下,镎稳定了 UO2 型萤石结构;(ii)在很宽的组成范围内观察到 U3O8 型正交相结构。我们明确证明了在这一相中的镎掺入,这在以前的研究中一直是一个有争议的问题。我们认为,镎的四价状态的特殊稳定性是导致观察到的相关系的原因。