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Surface-diffusion studies on UO2 and MgO

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Abstract

An optical interferometric technique has been used to study the growth of grain boundary grooves and the decay of surface scratches on UO2 and MgO at temperatures in the range 1100 to 1700° C. The results were interpreted using equations derived by W. W. Mullins and it was found that surface-diffusion was the predominant material transport process for both oxides under the experimental conditions used. Surface-diffusion coefficients and activation energies were calculated, and gave the following equations for the variation of the mass transfer surface-diffusion coefficientD s with temperature.

$$\begin{gathered} UO_{2.005, } {\text{ }}D_s = 1.3 x 10^8 exp^{ - 11000 \pm 15000} /RT[1200{\text{ to }}1{\text{400}}^\circ {\text{ C]}} \hfill \\ MgO, D_s = 8 x 10^4 exp^{ - 88500 \pm 15000} /RT[1200{\text{ to }}15{\text{00}}^\circ {\text{ C]}} \hfill \\ \end{gathered}$$

It was found that for UO2 the rate of grooving increased markedly as the oxygen content of the oxide increased.

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First read at an International Symposium on Reaction Mechanisms of Inorganic Solids, a meeting arranged by the Chemical Society and held at the University of Aberdeen, 11–16 July 1966.

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Henney, J., Jones, J.W.S. Surface-diffusion studies on UO2 and MgO. J Mater Sci 3, 158–164 (1968). https://doi.org/10.1007/BF00585483

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