Article ID Journal Published Year Pages File Type
1523994 Materials Chemistry and Physics 2012 6 Pages PDF
Abstract
► Sillenite Bi25FeO40 is the intermediate phase in the formation of pervoskite BiFeO3. ► Phase evolution can be controlled by adjusting the process parameters. ► The dissolution of Fe(OH)3 plays an important role to control the phase evolution of bismuth ferrites. ► The formation of perovskite BiFeO3 crystallites was based on the dissolution of sillenite Bi25FeO40.
Related Topics
Physical Sciences and Engineering Materials Science Electronic, Optical and Magnetic Materials
Authors
, , , , , ,