Evolution of Magnetic Symmetry through the BiFeO<sub>3</sub>-Ca<sub>2</sub>Fe<sub>4/3</sub>W<sub>2/3</sub>O<sub>6</sub> Phase Diagram.
Ontology highlight
ABSTRACT: Perovskites offer vast flexibility in tuning subtle distortions in their structures through their innate ability to host a wide range of compositional combinations. Minor changes in composition can dramatically influence the properties observed through structural distortions such as octahedral tilting. In addition to understanding their properties, in magnetic materials, the magnetic structure is also tied to the nuclear structural distortions and can have more complex behavior with changing composition. In this work we report on the magnetic properties, and nuclear and magnetic structures of the solid solution (1 - x)BiFeO3 - (x/2)Ca2Fe4/3W2/3O6. With the exception of BiFeO3, all samples show a weak ferromagne
SUBMITTER: Crawford CA
PROVIDER: S-EPMC12326346 | biostudies-literature | 2025 Aug
REPOSITORIES: biostudies-literature
ACCESS DATA