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二氧化铀氧化的密度泛函理论计算:UO(2+x)、U4O(9-y)、U3O7 和 U3O8 的演化。

Density functional theory calculations of UO2 oxidation: evolution of UO(2+x), U4O(9-y), U3O7, and U3O8.

机构信息

Materials Science and Technology Division, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, United States.

出版信息

Inorg Chem. 2013 Mar 4;52(5):2769-78. doi: 10.1021/ic400118p. Epub 2013 Feb 13.

DOI:10.1021/ic400118p
PMID:23406007
Abstract

Formation of hyperstoichiometric uranium dioxide, UO2+x, derived from the fluorite structure was investigated by means of density functional theory (DFT) calculations. Oxidation was modeled by adding oxygen atoms to UO2 fluorite supercells. For each compound ab initio molecular dynamics simulations were performed to allow the ions to optimize their local geometry. A similar approach was used for studying the reduction of U3O8. In agreement with the experimental phase diagram we identify stable line compounds at the U4O9-y and U3O7 stoichiometries. Although the transition from fluorite to the layered U3O8 structure occurs at U3O7 (UO2.333) or U3O7.333 (UO2.444), our calculated low temperature phase diagram indicates that the fluorite derived compounds are favored up to UO2.5, that is, as long as the charge-compensation for adding oxygen atoms occurs via formation of U(5+) ions, after which the U3O8-y phase becomes more stable. The most stable fluorite UO2+x phases at low temperature (0 K) are based on ordering of split quad-interstitial oxygen clusters. Most existing crystallographic models of U4O9 and U3O7, however, apply the cuboctahedral cluster. To better understand these discrepancies, the new structural models are analyzed in terms of existing neutron diffraction data. DFT calculations were also performed on the experimental cuboctahedral based U4O9-y structure, which enable comparisons between the properties of this phase with the quad-interstitial ones in detail.

摘要

通过密度泛函理论(DFT)计算研究了富铀二氧化物 UO2+x 的形成,该物质源自萤石结构。通过向 UO2 萤石超胞中添加氧原子来模拟氧化。对于每个化合物,都进行了从头算分子动力学模拟,以使离子能够优化其局部几何形状。类似的方法也用于研究 U3O8 的还原。与实验相图一致,我们确定了 U4O9-y 和 U3O7 化学计量的稳定线化合物。尽管从萤石到层状 U3O8 结构的转变发生在 U3O7(UO2.333)或 U3O7.333(UO2.444),但我们计算的低温相图表明,在 UO2.5 之前,即只要通过形成 U(5+) 离子来补偿添加氧原子的电荷,富铀萤石衍生化合物是有利的,之后 U3O8-y 相变得更稳定。低温(0 K)下最稳定的富铀萤石 UO2+x 相基于分裂四间隙氧团簇的有序排列。然而,大多数现有的 U4O9 和 U3O7 晶体学模型都应用了立方八面体簇。为了更好地理解这些差异,根据现有的中子衍射数据分析了新的结构模型。还对实验立方八面体基 U4O9-y 结构进行了 DFT 计算,这使得可以详细比较该相和四间隙相的性质。

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