Comment on "Modeling oxygen self-diffusion in UO2 under pressure by M.W.D Cooper et al., Solid State Ionics 282 (2015) 26-30"
N. V. Sarlis, E. S. Skordas

TL;DR
This paper extends previous studies on oxygen self-diffusion in UO2 under pressure, revealing that the activation volume's compressibility is much higher than that of the bulk, challenging common assumptions.
Contribution
It provides new insights into the compressibility of activation volumes in UO2, showing they differ significantly from bulk material properties.
Findings
Activation volume compressibility exceeds bulk compressibility by nearly an order of magnitude.
The thermal expansion coefficient of the activation volume differs from that of the bulk.
This challenges the common assumption that activation volume and bulk compressibility are equal.
Abstract
The oxygen self-diffusion coefficient in UO has been recently studied [Cooper et al. Solid State Ionics 282 (2015) 26-30] over a range of pressures (0-10GPa) and temperatures (300-1900K) by combining molecular dynamics calculations with a thermodynamical model, the cB{\Omega} model. A significant reduction in oxygen self-diffusion as a function of increasing hydrostatic pressure, and the associated increase in activation energy was identified. Here, we extend this study and find that the compressibility of the corresponding activation volume exceeds significantly the compressibility of the bulk material by almost one order of magnitude. This results is important since in the literature it is usually assumed that these two compressibilities are equal. The same holds when comparing the thermal expansion coefficient of this volume with that of the bulk solid.
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Taxonomy
TopicsAdvanced Condensed Matter Physics · Advancements in Solid Oxide Fuel Cells · High-pressure geophysics and materials
