Abstract
The monoclinic β-polymorph of gallium oxide is a semiconductor with an ultra-wide bandgap. It is becoming increasingly significant for various technological applications. We have investigated the tracer self-diffusion of oxygen in β-Ga2O3 single crystals as a function of the oxygen partial pressure (2, 20 and 200 mbar) at a temperature of 1375 °C. Isotopically enriched 18O2 gas was used as a tracer source and secondary ion mass spectrometry to analyze depth profiles. We observed that, with decreasing oxygen partial pressure, the diffusivities at a given temperature increase significantly. We suggest that this behaviour can be explained by a change in the diffusion mechanism from oxygen interstitials to oxygen vacancies.
Dedicated to Professor Thomas Bredow of the University of Bonn on the occasion of his 60th birthday.
Acknowledgments
This work was funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – SCHM – 15619/35-1. This financial support is gratefully acknowledged.
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Research ethics: Noted and followed.
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Author contribution: The authors have accepted responsibility for the entire content of this manuscript and approved its submission.
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Competing interests: The authors states no conflict of interest.
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Research funding: Funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – SCHM – 15619/35-1.
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Data availability: The raw data can be obtained on request from the corresponding author.
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