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Hydrogen incorporation and diffusion in fluorite PuO2

Andrew J. E. Rowberg*, Kyoung E. Kweon, and Scott B. Donald

  • *Contact author: rowberg1@llnl.gov

Phys. Rev. Materials 10, L102401 – Published 5 October, 2026

DOI: https://doi.org/10.1103/fvxz-v6tj

Abstract

Hydriding is a primary degradation mode of plutonium metal, and although it tends to be mitigated by the presence of the native surface oxide, the degree of protection depends heavily on the oxide chemistry. Here, we use hybrid density-functional theory calculations to evaluate the thermodynamics and kinetics of hydrogen in PuO2 as a function of environmental oxygen content. Under O-rich conditions, hydrogen will incorporate primarily through interstitial protons Hi+, which peak in concentration at 1016 cm−3. Hi+ has very small kinetic barriers (<0.1eV), although its diffusion will be limited by its small concentrations. For more O-poor conditions, hydrogen prefers to substitute for oxygen as HO; this species can reach concentrations exceeding 1020 cm−3. HO diffuses into neighboring oxygen vacancies VO with barriers between 0.39–0.71 eV, depending on the charge state of VO. These barriers will be overcome readily at room temperature. In addition, as conditions become increasingly O-poor, electron polarons η− will form in higher concentrations, reflecting reduction from Pu4+ to Pu3+. These species will tend to reduce Coulombic repulsion between HO and VO, resulting in faster diffusion. Our results provide important insights into the properties of hydrogen in plutonium oxides, which dictate the critical process of hydriding.

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