Figure 9. An Auger spectrum of O KLL from a UO2 film (sample AP3). CONCLUSIONS




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Figure 9. An Auger spectrum of O KLL from a UO2 film (sample AP3).





CONCLUSIONS

XPS determination of the oxygen coefficient kO=2+x and ionic (U4+, U5+ and U6+) composition of oxides UO2+x formed on the surfaces of differently oriented (hkl) planes of thin UO2 films on the LSAT and YSZ substrates was performed. The U 4f and O 1s core-electron peak intensities as well as the U 5f relative intensity before and after the 129Xe23+ (92 MeV, fluence 4.8×1015 ions/cm2) and 238U31+ (110 MeV, fluence 5×1010, 5×1011 and 5×1012 ions/cm2) irradiations were employed.

It was found that the presence of uranium dioxide film in air results in formation of oxide UO2+x on the surface with mean oxygen coefficients kO from 2.07 to 2.11 on the LSAT and from 2.17 to 2.23 on the YSZ substrates. These oxygen coefficients depend on the nature of the substrate and weakly on the crystallographic orientation.

On the basis of the spectral parameters it was established that uranium dioxide films AP2,3 on the LSAT substrates have closest to stoichiometric values of the kO, and from the XRD and EBDS results it follows that these films have a regular single crystal structure. The XRD and EBSD results indicate that uranium oxide films on the YSZ substrates have single crystal structure, however, they have the highest oxygen coefficient kO. This difference, possibly, related to the different nature of the substrates.

The 129Xe23+ irradiation (92 MeV, fluence 4.8×1015 ions/cm2) of uranium dioxide films on the LSAT substrates was shown to destroy both long range ordering and uranium close environment, which results in increase of uranium oxidation state and regrouping of oxygen ions in the uranium close environment. The 238U31+ irradiations (110 MeV, fluence 5×1010, 5×1011 and 5×1012 ions/cm2) of uranium dioxide films on the YSZ substrates was shown to form the lattice damage only with partial destruction of the long range ordering. This is mainly due to low fluencies. However, the 238U31+ irradiations caused changes in the ionic composition of the samples: an increase in U4+ concentration and a decrease in U6+ concentration were observed, hence the oxygen coefficient (kO) decreased compared to that for the unirradiated counter-parts.



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Figure 9. An Auger spectrum of O KLL from a UO2 film (sample AP3). CONCLUSIONS

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