Abstract

We studied the electronic structure of granular Fe–Al 2O 3 thin films using X-ray photoelectron spectroscopy (XPS). The samples were produced by co-evaporation of Fe and Al 2O 3 and have relatively large Fe volume factions (27 and 48%). The Fe 2p XPS spectra show that the Fe precipitates in the granular alloy are in a majority metallic phase. The spectra show also that there is a minority Fe oxide phase and that this phase decreases for the 48% sample. The valence band spectra of granular Fe–Al 2O 3 can be understood as a linear combination of the individual Fe and Al 2O 3 bands, which is consistent with mostly metallic Fe precipitates deduced from the core level Fe 2p XPS spectra. The core level and valence band results suggest the possibility of little interaction between the Fe precipitates and the Al 2O 3 matrix. In turn, this would suggest that there is little interdiffusion as well as relatively well-defined and abrupt grain boundaries. This information is important to understand the transport and magnetic properties of the Fe–Al 2O 3 thin films.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.