ErFeO3 ceramics had been synthesized by the solid-state reaction method at a variety of sintering temperatures (1250, 1300, 1350, 1400, 1450, and 1500 °C). The microstructure, surface morphology, and elemental valence state of ErFeO3 polycrystalline ceramics were investigated using X-ray diffraction (XRD), Raman spectroscopy (Raman), scanning electron microscopy (SEM), and X-ray photoelectron spectroscopy (XPS). The study discovered that Fe3+ ions keep their valence, and all samples at temperatures ranging from 1300 to 1450 °C are in a pure phase. Within this range, increasing temperature widens the Fe-O-Fe bond angle, lengthens the Er-O bond, suppresses the super-exchange contact between the two ions via O2−, and diminishes the electromagnetic coupling effect. A Physical Property Measurement System (PPMS) was utilized to assess the magnetic properties of ErFeO3 polycrystalline ceramics. Ceramic samples sintered at 1300 °C showed spontaneous spin reorientation and a shift from ionic magnetic disorder to magnetic order. The magnetic hysteresis loops at temperatures before and after spin reorientation were examined. It was noted that the polycrystalline ceramic ErFeO3 underwent a transition in its magnetic configuration from Γ4 (Gx, Ay, Fz) to Γ2 (Fx, Cy, and Gz). As the sintering temperature increases, ErFeO3 polycrystalline ceramics lose their temperature adjustment point. This disrupts the spin reorientation of Er3+ and Fe3+ magnetic moments in the 89–102 K region. The secondary phase transition of ErFeO3 polycrystalline ceramics causes disorder, and the Néel temperature of Er3+ rises. This suggests that the sublattice field and magnetic ordering of Er3+ and Fe3+ are disturbed when the sintering temperature is raised. Consequently, 1300 °C is the optimal sintering temperature for ErFeO3 polycrystalline ceramics.
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