Abstract

The antipolar orthorhombic Pnma phase with the 2 a p × 4 a p × 2 2 a p superstructure (ap ~4 Å is the pseudocubic perovskite unit-cell parameter) is observed in many perovskite compositions derived from BiFeO3. Temperature-induced structural transformations in metastable perovskite solid solutions with the Pnma structure corresponding to the range of 0.30 ≤ y ≤ 0.60 of the (1−y)BiFeO3-yBiScO3 quasi binary system were studied using temperature X-ray and neutron powder diffraction. These compositions cannot be prepared in bulk form at ambient pressure but can be stabilized in the Pnma phase by means of quenching after synthesis under high pressure. The compositions were investigated in situ between 1.5 K and the temperature of the stability limit of their metastable phases (about 870–920 K). It has been found that heating the as-prepared compositions with the Pnma phase leads to formation of the rhombohedral R3c phase ( 2 a p × 2 a p × 2 3 a p ), which, on cooling down to room temperature, either remains or transforms into a polar orthorhombic Ima2 phase ( 2 a p × 2 a p × 2 a p ). The observed phase transformations in the BiFe1−yScyO3 perovskite series on heating and on cooling are considered in terms of geometrical factors.

Highlights

  • Perovskite multiferroics based on chemically modified bismuth ferrite attract great attention in respect to both fundamental research and practical application [1,2]

  • We report on the temperature behaviour of the metastable perovskite phases of the BiFe1−y Scy O3 series studied using in situ powder X-ray and neutron diffraction

  • The perovskite compositions of the BiFe1−y Scy O3 series (0.30 ≤ y ≤ 0.60) prepared using a high-pressure synthesis are orthorhombic with the antipolar Pnma structure

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Summary

Introduction

Perovskite multiferroics based on chemically modified bismuth ferrite attract great attention in respect to both fundamental research and practical application [1,2]. While the conventional preparation methods are generally applicable to obtain bulk polycrystalline samples with the entire range of the Bi-site substitutions, a wide range of Fe-site substitutions are possible under high pressure only. The high-pressure synthesis technique offers unique opportunities to obtain new phases but requires complicated and expensive equipment. A sample obtained as a result of one high-pressure high-temperature run, is rather small. In cases when the required pressure is above. The cases when researchers managed to measure dielectric properties of the high-pressure synthesized ceramics are rather rare [3,4,5,6,7]

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