Limits of Solid Solution and Evolution of Crystal Morphology in (La1-XREX)FeO3 Perovskites by Low Temperature Hydrothermal Crystallization

The crystallization of a new series of A-site substituted lanthanum ferrite materials (La1-xREx)FeO3 was explored by the hydrothermal method at 240 degrees C, for rare earth (RE) = Nd, Sm, Gd, Ho, Er, Yb, and Y, with 0 < x < 1. The effect of elemental substitution on the morphological, structural, and magnetic properties of the materials was studied using high-resolution powder X-ray diffraction, energy dispersive spectroscopy (EDS) on the scanning electron microscope, Raman spectroscopy, and SQUID magnetometry. If the radius of the La3+ and the substituent ions is similar, such as for Nd3+, Sm3+, and Gd3+, homogeneous solid solutions are formed, with the orthorhombic GdFeO3-type structure, and a continuous evolution of Raman spectra with composition and distinct magnetic behavior from the end members. When the radius difference between substituents and La3+ is large, such as for Ho3+, Er3+, Yb3+, and Y3+, then instead of forming solid solutions, crystallization in separate phases is found. However, low levels of element mixing are found and intergrowths of segregated regions give composite particles. In this case, the Raman spectra and magnetic behavior are characteristic of mixtures of phases, while EDS shows distinctive elemental segregation. A-site replacement induces an evolution in the crystallite shape with an increasing amount of substituent ions and this is most evident for RE = Y from cube-shaped crystals seen for LaFeO3 to multipodal crystals for (La1-xYx)FeO3, providing evidence for a phase-separation-driven evolution of morphology.

Automated summary

In this study, the crystallization of a new series of A-site substituted lanthanum ferrite materials (La1-xREx)FeO3 was explored using hydrothermal method. The effect of elemental substitution on the morphological, structural, and magnetic properties of the materials was studied. It was found that homogeneous solid solutions are formed when La3+ and substituent ions have similar radii, while crystallization in separate phases is found when there is a large radius difference. A-site replacement induces an evolution in the crystallite shape, providing evidence for a phase-separation-driven evolution of morphology.