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六氟化铀水解的理论研究:引发机制与振动光谱

A theoretical investigation of the hydrolysis of uranium hexafluoride: the initiation mechanism and vibrational spectroscopy.

作者信息

Lutz Jesse J, Byrd Jason N, Lotrich Victor F, Jensen Daniel S, Zádor Judit, Hubbard Joshua A

机构信息

Center for Computing Research (CCR), Sandia National Laboratories, Albuquerque, New Mexico, USA.

ENSCO, Inc., 4849 North Wickham Road, Melbourne, Florida, 32940, USA.

出版信息

Phys Chem Chem Phys. 2022 Apr 20;24(16):9634-9647. doi: 10.1039/d1cp05268c.

DOI:10.1039/d1cp05268c
PMID:35404371
Abstract

Depleted uranium hexafluoride (UF), a stockpiled byproduct of the nuclear fuel cycle, reacts readily with atmospheric humidity, but the mechanism is poorly understood. We compare several potential initiation steps at a consistent level of theory, generating underlying structures and vibrational modes using hybrid density functional theory (DFT) and computing relative energies of stationary points with double-hybrid (DH) DFT. A benchmark comparison is performed to assess the quality of DH-DFT data using reference energy differences obtained using a complete-basis-limit coupled-cluster (CC) composite method. The associated large-basis CC computations were enabled by a new general-purpose pseudopotential capability implemented as part of this work. Dispersion-corrected parameter-free DH-DFT methods, namely PBE0-DH-D3(BJ) and PBE-QIDH-D3(BJ), provided mean unsigned errors within chemical accuracy (1 kcal mol) for a set of barrier heights corresponding to the most energetically favorable initiation steps. The hydrolysis mechanism is found to proceed intermolecular hydrogen transfer within van der Waals complexes involving UF, UFOH, and UOF, in agreement with previous studies, followed by the formation of a previously unappreciated dihydroxide intermediate, UF(OH). The dihydroxide is predicted to form under both kinetic and thermodynamic control, and, unlike the alternate pathway leading to the UOF monomer, its reaction energy is exothermic, in agreement with observation. Finally, harmonic and anharmonic vibrational simulations are performed to reinterpret literature infrared spectroscopy in light of this newly identified species.

摘要

六氟化贫铀(UF)是核燃料循环中储存的一种副产品,它能迅速与大气湿度发生反应,但其反应机制尚不清楚。我们在一致的理论水平上比较了几个潜在的引发步骤,使用混合密度泛函理论(DFT)生成基础结构和振动模式,并使用双杂化(DH)DFT计算驻点的相对能量。使用通过完整基组极限耦合簇(CC)复合方法获得的参考能量差进行基准比较,以评估DH-DFT数据的质量。作为本工作的一部分,新实现的一种通用赝势功能实现了相关的大基组CC计算。色散校正的无参数DH-DFT方法,即PBE0-DH-D3(BJ)和PBE-QIDH-D3(BJ),对于一组对应于能量最有利引发步骤的势垒高度,提供了化学精度(1 kcal/mol)内的平均绝对误差。水解机制被发现是在涉及UF、UFOH和UOF的范德华复合物内进行分子间氢转移,这与之前的研究一致,随后形成一种之前未被重视的二氢氧化物中间体UF(OH)₂。预计二氢氧化物在动力学和热力学控制下均能形成,并且与导致UOF单体的替代途径不同,其反应能量是放热的,这与观察结果一致。最后,进行了谐波和非谐波振动模拟,以便根据这个新发现的物种重新解释文献中的红外光谱。

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