Successive spin reorientation and rare earth ordering in NdDyFeO: Experimental and - investigations
arXiv:1904.05837 · doi:10.1103/PhysRevB.102.144432
Abstract
In present study, the magnetic structure and spin reorientation of mixed doped orthoferrite NdDyFeO have been investigated. Similar to both parent compounds (NdFeO and DyFeO), the magnetic structure of Fe belongs to irreducible representation (G, F) at room temperature. The experimental measurements confirmed the spin reorientation where magnetic structure of Fe changes from to (F, G) between 75 and 20 \,K while maintaining G-type configuration. Such a gradual spin reorientation is unusual since the large single ion anisotropy of Dy ions causes an abrupt (G) spin reorientation in DyFeO. Between 20 and 10 \,K, the Fe magnetic structure is represented by (F, G). Unexpectedly, magnetic structure of Fe with representation re-emerges below 10\,K which also coincides with the development of rare-earth (Nd/Dy) magnetic ordering having C configuration with magnetic moment of 1.8 . The absence of any signature of second order phase transition in the specific heat confirms the role of (Nd/Dy)-Fe exchange interaction in the observed "rare-earth ordering" unlike DyFeO where Dy ordering takes place independently to the magnetic ordering of Fe magnetic structure. Our (DFT+U+SO) calculations show that the C-type arrangement of rare-earth ions (Nd/Dy) with configuration for Fe moments is the ground state whereas phase is energetically very close. Nd-Fe and Nd-Dy exchange interactions, estimated from DFT, are observed to have significant roles in the rare earth ordering and Fe spin reorientation corroborating our experimental results.
arXiv comment11 pages, 11 figures
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