Spin and lattice dynamics at the spin-reorientation transitions in the rare-earth orthoferrite Sm$_{0.55}$Tb$_{0.45}$FeO$_{3}$
R. M. Dubrovin, A. I. Brulev, N. R. Vovk, I. A. Eliseyev, N. N. Novikova, V. A. Chernyshev, A. N. Smirnov, V. Yu. Davydov, Anhua Wu, Liangbi Su, R. V. Mikhaylovskiy, A. M. Kalashnikova, R. V. Pisarev
TL;DR
This study investigates spin and lattice dynamics at spin-reorientation transitions in the mixed rare-earth orthoferrite Sm$_{0.55}$Tb$_{0.45}$FeO$_3$ using polarized infrared reflectivity and Raman spectroscopy, complemented by first-principles lattice-dynamics calculations. It identifies two spin-reorientation temperatures, $T_{1} \approx 220$ K and $T_{2} \approx 130$ K, between Γ$_4$, Γ$_{24}$, and Γ$_2$ magnetic structures, with an unusually wide intermediate Γ$_{24}$ phase ($\Delta T \approx 90$ K) attributed to inhomogeneous magnetocrystalline anisotropy from Sm/Tb disorder. Raman measurements reveal two magnon modes, qFM ≈ 7 cm$^{-1}$ and qAFM ≈ 18 cm$^{-1}$, whose intensities and frequencies evolve with temperature and magnetic structure; the qFM mode softens but retains a magnetoelastic gap (~6 cm$^{-1}$), while no new Raman-active phonons appear across the transitions. Infrared-active phonons and Raman-active phonons largely follow calculated predictions, with no evidence for spin-phonon coupling or defect-induced phonons at the transitions. The results advance understanding of magnetophononic phenomena in rare-earth orthoferrites and show how compositional disorder can tune spin-reorientation temperatures, informing potential temperature-controlled magnetic devices.
Abstract
Linear and non-linear couplings of magnetic and lattice excitations are at the heart of many fascinating magnetophononic phenomena observed in rare-earth orthoferrites, the distinctive feature of which is the tendency to spin-reorientation transitions. Here we report the results of the experimental study of the spin and lattice dynamics in the Brillouin zone center of the rare-earth orthoferrite Sm$_{0.55}$Tb$_{0.45}$FeO$_{3}$ by using polarized infrared reflectivity and Raman scattering spectroscopic techniques. The obtained results were supported by the first-principles calculations, which allowed us to reliably identify the parameters of most infrared- and Raman-active phonons. We reveal the spin-reorientation transitions $Γ_{4}(G_{a}F_{c}) \overset{T_{1}}\longleftrightarrow Γ_{24}(G_{ac}F_{ac}) \overset{T_{2}}\longleftrightarrow Γ_{2}(G_{c}F_{a})$ at $T_{1} \simeq 220$ K and $T_{2} \simeq 130$ K and carefully studied the following evolution of Raman scattering on magnetic excitations at these transitions. Notably, the intermediate magnetic structure $Γ_{24}$ displays an exceptionally broad temperature range $Δ{T} = T_{1} - T_{2} \simeq 90$ K in mixed Sm$_{0.55}$Tb$_{0.45}$FeO$_{3}$ compared to pure rare-earth orthoferrites. We attribute this broadening of the intermediate phase to the modification of the magnetocrystalline anisotropy as a result of the inhomogeneous magnetic structure caused by the random distribution of rare-earth $\mathrm{Sm}^{3+}$ and $\mathrm{Tb}^{3+}$ ions. We found neither change in the parameters of Raman-active $B_{1g}$ phonons nor the appearance of new phonons induced by spin-reorientation transitions, which have been reported in $\mathrm{SmFeO}_{3}$. We assume that our results provide a solid basis for more deeper understanding of magnetophononic phenomena in rare-earth orthoferrites.
