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层状氢氧化铀(VI):脱水柱铀矿α-UO₂(OH)₂的结构和热力学性质

Layered uranium(VI) hydroxides: structural and thermodynamic properties of dehydrated schoepite α-UO₂(OH)₂.

作者信息

Weck Philippe F, Kim Eunja

机构信息

Sandia National Laboratories, Albuquerque, NM 87185, USA.

出版信息

Dalton Trans. 2014 Dec 7;43(45):17191-9. doi: 10.1039/c4dt02455a.

DOI:10.1039/c4dt02455a
PMID:25318965
Abstract

The structure of dehydrated schoepite, α-UO2(OH)2, was investigated using computational approaches that go beyond standard density functional theory and include van der Waals dispersion corrections (DFT-D). Thermal properties of α-UO2(OH)2, were also obtained from phonon frequencies calculated with density functional perturbation theory (DFPT) including van der Waals dispersion corrections. While the isobaric heat capacity computed from first-principles reproduces available calorimetric data to within 5% up to 500 K, some entropy estimates based on calorimetric measurements for UO3·0.85H2O were found to overestimate by up to 23% the values computed in this study.

摘要

使用超越标准密度泛函理论并包含范德华色散校正(DFT-D)的计算方法,对脱水柱铀矿α-UO₂(OH)₂的结构进行了研究。α-UO₂(OH)₂的热性质也通过密度泛函微扰理论(DFPT)计算的声子频率获得,该理论包含范德华色散校正。虽然从第一性原理计算得到的等压热容在500 K以下能将现有量热数据重现至5%以内,但发现一些基于UO₃·0.85H₂O量热测量的熵估计值比本研究计算的值高估了23%。

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