Pressure induced phase transitions in Sm-doped BiFeO3 in the morphotropic phase boundary
arXiv:2111.11167 · doi:10.1016/j.matchemphys.2021.125458
Abstract
Sm-doped BiFeO3 compacted powders with composition across the morphotropic phase boundary region were prepared by sol-gel method. Crystal structure, morphology and magnetic state of the compounds were analyzed as a function of dopant concentration, temperature and external pressure using synchrotron and laboratory X-ray diffraction, electron microscopy, Raman and Mossbauer spectroscopy. Application of external pressure shifts the phase transition from the rhombohedral structure to the nonpolar orthorhombic structure towards lower concentration of the dopant content, wherein the amount of the anti-polar orthorhombic phase notably decreases. Raman and Mossbauer spectroscopy data provides additional information about the structural distortion on local scale level which testifies faster formation of nonpolar orthorhombic phase and associated modification in the magnetic state in the compounds subjected to high pressure. Temperature increase leads to the structural transition to the nonpolar orthorhombic phase regardless the structural state at room temperature; furthermore, application of external pressure decreases the phase transition temperature.
References in corpus (6)
- Weak ferromagnetism and magnetoelectric coupling in bismuth ferrite
- Origin of magnetoelectric behavior in BiFeO
- Room temperature coexistence of large electric polarization and magnetic order in BiFeO3 single crystals
- Nanoscale ferroelectricity in pseudo-cubic sol-gel derived barium titanate -- bismuth ferrite (BaTiO-BiFeO) solid solutions
- Evolution of the crystal structure and magnetic properties of Sm-doped BiFeO3 ceramics across the phase boundary region
- First principle study of crystal growth morphology: An application to crystalline urea