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Main Authors: Zhang, Xue-Jing, Koch, Erik, Pavarini, Eva
Format: Preprint
Published: 2024
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Online Access:https://arxiv.org/abs/2411.16351
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author Zhang, Xue-Jing
Koch, Erik
Pavarini, Eva
author_facet Zhang, Xue-Jing
Koch, Erik
Pavarini, Eva
contents The surprising inversion of the orbital- and magnetic-order transition temperatures in the RVO3 series with increasing the rare-earth radius makes the series unique among orbitally-ordered materials. Here, augmenting dynamical mean-field theory with a decomposition of the order parameter into irreducible tensors, we show that this anomalous behavior emerges from an unusual hierarchy of interactions. First, increasing the rare-earth radius, orbital physics comes to be controlled by xz-xz quadrupolar super-exchange rather than by lattice distortion. Next, for antiferromagnetic spin order, orbital super-exchange terms with different spin rank compete, so that the dipolar spin-spin interaction dominates. Eventually, G-type magnetic order (anti-ferro in all directions) can appear already above the orbital ordering transition, and C-type order (anti-ferro in the ab plane) right around it. The strict constraints we found explain why the inversion is rare, giving at the same time criteria to look for similar behavior in other materials.
format Preprint
id arxiv_https___arxiv_org_abs_2411_16351
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Origin of the transitions inversion in rare-earth vanadates
Zhang, Xue-Jing
Koch, Erik
Pavarini, Eva
Strongly Correlated Electrons
Materials Science
The surprising inversion of the orbital- and magnetic-order transition temperatures in the RVO3 series with increasing the rare-earth radius makes the series unique among orbitally-ordered materials. Here, augmenting dynamical mean-field theory with a decomposition of the order parameter into irreducible tensors, we show that this anomalous behavior emerges from an unusual hierarchy of interactions. First, increasing the rare-earth radius, orbital physics comes to be controlled by xz-xz quadrupolar super-exchange rather than by lattice distortion. Next, for antiferromagnetic spin order, orbital super-exchange terms with different spin rank compete, so that the dipolar spin-spin interaction dominates. Eventually, G-type magnetic order (anti-ferro in all directions) can appear already above the orbital ordering transition, and C-type order (anti-ferro in the ab plane) right around it. The strict constraints we found explain why the inversion is rare, giving at the same time criteria to look for similar behavior in other materials.
title Origin of the transitions inversion in rare-earth vanadates
topic Strongly Correlated Electrons
Materials Science
url https://arxiv.org/abs/2411.16351