Abstract
A high-temperature X-ray diffraction method is used under controlled pressure to evaluate dependence of the lattice parameter of various oxides at 700 and 1000 °C on the partial pressures of oxygen. Fe 1− x O and CoO have complete mutual solubility at 1000 °C. Two monoxides are observed at 700 °C. The solubility of cobalt in iron protoxide is weak; the solubility of iron decreases with increasing oxygen partial pressures in cobalt monoxide. They are respectively in the c.c. alloy and spinel phase.
Sign-in/Register to access full text options 
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 callDisclaimer: 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.
