Abstract

Uranium speciation and redox behaviour is of critical importance in the nuclear fuel cycle. X-ray absorption near-edge spectroscopy (XANES) is commonly used to probe the oxidation state and speciation of uranium, and other elements, at the macroscopic and microscopic scale, within nuclear materials. Two-dimensional (2D) speciation maps, derived from microfocus X-ray fluorescence and XANES data, provide essential information on the spatial variation and gradients of the oxidation state of redox active elements such as uranium. In the present work, we elaborate and evaluate approaches to the construction of 2D speciation maps, in an effort to maximize sensitivity to the U oxidation state at the U L3-edge, applied to a suite of synthetic Chernobyl lava specimens. Our analysis shows that calibration of speciation maps can be improved by determination of the normalized X-ray absorption at excitation energies selected to maximize oxidation state contrast. The maps are calibrated to the normalized absorption of U L3 XANES spectra of relevant reference compounds, modelled using a combination of arctangent and pseudo-Voigt functions (to represent the photoelectric absorption and multiple-scattering contributions). We validate this approach by microfocus X-ray diffraction and XANES analysis of points of interest, which afford average U oxidation states in excellent agreement with those estimated from the chemical state maps. This simple and easy-to-implement approach is general and transferrable, and will assist in the future analysis of real lava-like fuel-containing materials to understand their environmental degradation, which is a source of radioactive dust production within the Chernobyl shelter.

Highlights

  • Understanding uranium redox behaviour in materials generated in the nuclear fuel cycle and, importantly, those formed during nuclear accidents, is essential when developing effective remediation strategies to mitigate the impact of this radioactive element in the environment

  • The correlation of U and Zr distributions are in excellent agreement with the previous study of phase assemblages obtained by a combination of m-X-ray diffraction (XRD) and m-X-ray fluorescence (XRF) analysis (Ding et al, 2021)

  • The distribution of Fe and Ni was concentrated in Fe–Ni alloy particles, as observed in a previous study (Ding et al, 2021); an example is shown in the approximate centre of the m-XRF maps shown in Fig. 2, between the edges of two neighbouring crystallites

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Summary

Introduction

Understanding uranium redox behaviour in materials generated in the nuclear fuel cycle and, importantly, those formed during nuclear accidents, is essential when developing effective remediation strategies to mitigate the impact of this radioactive element in the environment. U6+ is prevalent in oxidizing conditions, with a higher solubility, for example in oxic groundwater. Predominantly UO2, exhibits extremely low corrosion rates in groundwater under anoxic conditions; the corrosion rate increases significantly when oxidative corrosion occurs, i.e. oxidation of U4+ to U6+ by oxidative and radiolytic solution species (Shoesmith, 2000). It has been shown that borosilicate glass immobilizing U3O8 exhibited leaching rates in oxic ground water that were four times higher than in anoxic. The oxidation state of U within the material itself has been found to influence corrosion rates; for borosilicate and aluminosilicate glasses immobilizing U, those with a higher mean oxidation state demonstrated the greatest extent of U release (Barlow et al, 2021)

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