SrV 0.3 Fe 0.7 O 2.8 : A Vacancy-Ordered Fe-Based Perovskite Exhibiting Room-Temperature Magnetoresistance.
Teppei NagaseTakumi NishikuboMasayuki FukudaYuki SakaiKei ShigematsuYoichi IkedaYusuke NambuQiang ZhangMasaaki MatsudaKo MibuMasaki AzumaTakafumi YamamotoPublished in: Inorganic chemistry (2022)
We report room-temperature (RT) magnetoresistance (MR) in a novel Fe-based perovskite, SrV 0.3 Fe 0.7 O 2.8 . This compound contains ordered oxygen vacancies in every fifth primitive perovskite (111) p plane, leading to a layered structure consisting of triple-octahedral and double-tetrahedral layers. Along with the oxygen vacancies, the transition-metal ions are also ordered: the octahedral sites are occupied by 100% of Fe ions, while the tetrahedral sites are occupied by 25% of Fe ions and 75% of V ions. As a result, SrV 0.3 Fe 0.7 O 2.8 forms a magnetically striped lattice in which the octahedral layers with 100% of magnetic Fe ions are separated by the diluted magnetic layer. The compound exhibits weak ferromagnetism and shows a large negative MR (-5% at 3 T) at RT, despite the small saturation moment (0.4 μ B /Fe atom). Thus, this type of layered compound is promising for further large MR by an increase of magnetization through chemical substitution.
Keyphrases
- room temperature
- aqueous solution
- ionic liquid
- quantum dots
- transition metal
- metal organic framework
- contrast enhanced
- magnetic resonance imaging
- molecularly imprinted
- visible light
- highly efficient
- mass spectrometry
- solar cells
- molecular dynamics
- tandem mass spectrometry
- ion batteries
- simultaneous determination
- liquid chromatography