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Temperature- and Composition-Driven Structural and Magnetic Transitions in High-Pressure Stabilized Perovskites Based on BiFeO$_3$

9O-01
Jul 10, 2025, 3:00 PM
15m
ORAL Topic 9 - Multifunctional magnetic materials (multiferroic, magnetoelastic, shape memory, …) Section S9

Speaker

Andrei Salak (University of Aveiro)

Description

Chemical modifications in the iron site of BiFeO$_3$ represent the direct approach to tune the magnetic behaviour of this material. However, using the conventional synthesis routes, it is possible to achieve the substitution rates of a few atomic percent only. Most of the reported single-phase BiFe$_{1−y}$B$^{3+}_{y}$O$_3$ perovskite compositions with $y > 0.1$ were prepared via high-pressure synthesis.

In high-pressure stabilized perovskite solid solutions of the BiFe$_{1−y}$Sc$_y$O$_3$ system, a series of structural transitions with increasing $y$ was found. Moreover, it was revealed that annealing of the as-prepared perovskite phases results in irreversible transformations into new structural phases with interesting combinations of ferroic orders [1]. In the $0.1 \leq y < 0.3$ range, some peculiarities of the temperature-dependent magnetic moment below $T_N$ were observed and associated with possible transitions between different antiferromagnetic structures corresponding to collinear, canted, and cycloidal spin arrangements [2]. Similar temperature anomalies of the magnetic behaviour below $T_N$ were then revealed in the Fe-rich compositional range of the BiFe$_{1−y}$[Zn$_{0.5}$Ti$_{0.5}$]$_y$O$_3$ perovskites [3].

We present the temperature and compositional behaviours of the crystal structure and the magnetic properties of the BiFe$_{1−y}$B$^{3+}_{y}$O$_3$ perovskites (where B$^{3+}$ = Ga, Co, Mn, Cr, [Zn$_{0.5}$Ti$_{0.5}$] and Sc) in the vicinity of parent bismuth ferrite. Among these, Cr$^{3+}$, Mn$^{3+}$, and Co$^{3+}$ are magnetic cations of transition metals from the same 3d series to which iron belongs, while Ga$^{3+}$, Sc$^{3+}$ and [Zn$_{0.5}$Ti$_{0.5}$]$^{3+}$ are non-magnetic. Besides, as compared with iron, gallium is smaller, scandium is considerably bigger, and [Zn$_{0.5}$Ti$_{0.5}$]$^{3+}$ is slightly bigger than Fe$^{3+}$ in octahedral coordination. The crystal structure sequences, phase diagrams and the $T_N(y)$ dependences are compared and discussed.

References

[1] D. D. Khalyavin et al., “The phenomenon of conversion polymorphism in Bi-containing metastable perovskites,” Chemical Communications, vol. 55, no. 32. Royal Society of Chemistry (RSC), pp. 4683–4686, 2019. https://doi.org/10.1039/c9cc00472f
[2] E. L. Fertman et al., “Magnetic Diagram of the High-Pressure Stabilized Multiferroic Perovskites of the BiFe1-yScyO3 Series,” Crystals, vol. 10, no. 10. MDPI AG, p. 950, Oct. 17, 2020. https://doi.org/10.3390/cryst10100950
[3] A. N. Salak et al., “Magnetic Behaviour of Perovskite Compositions Derived from BiFeO3,” Magnetochemistry, vol. 7, no. 11. MDPI AG, p. 151, Nov. 16, 2021. https://doi.org/10.3390/magnetochemistry7110151

Primary author

Andrei Salak (University of Aveiro)

Co-authors

Dr Dmitry Khalyavin (ISIS Facility, Rutherford Appleton Laboratory) Dr Olena Fertman (B. Verkin Institute for Low Temp. Physics & Eng. of NASU) Dr Alexey Fedorchenko (B.I. Verkin Institute for Low Temperature Physics and Engineering of NAS of Ukraine) Prof. Alexander Feher (Pavol Jozef Šafárik University in Košice, Faculty of Science, Institute of Physics) Erik Čižmár (Pavol Jozef Šafárik University in Košice, Faculty of Science, Institute of Physics)

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