Abstract
Thermogravimetric analysis has revealed that reduction of in occurs in two distinct steps on heating up to 930 °C. Whereas reduction to give SrO, and Cu is complete above 800 °C, a stable intermediate forms in the region between 250 and 450 °C. This has been identified as a new tetragonal phase, with unit-cell dimensions and The structure has been determined from powder x-ray-diffraction data and is related to (-type). Madelung energy, bond valence sum calculations, and F -XPS data clearly indicate that the ions occupy sites within the fluorite block insulating layers. This contrasts with the (-type) structure which is adopted by
- Received 24 February 1997
DOI:https://doi.org/10.1103/PhysRevB.56.2831
©1997 American Physical Society