Origin of metal-insulator transition in rare-earth Nickelates

Fuente: arXiv
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Autores principales: Acharya, Swagata, Tellekamp, Brooks, Jackson, Jerome, Pashov, Dimitar, Blackburn, Jeffrey L., Alberi, Kirstin, van Schilfgaarde, Mark
Formato: Preprint
Publicado: 2025
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author Acharya, Swagata
Tellekamp, Brooks
Jackson, Jerome
Pashov, Dimitar
Blackburn, Jeffrey L.
Alberi, Kirstin
van Schilfgaarde, Mark
author_facet Acharya, Swagata
Tellekamp, Brooks
Jackson, Jerome
Pashov, Dimitar
Blackburn, Jeffrey L.
Alberi, Kirstin
van Schilfgaarde, Mark
contents Rare-earth nickelates RNiO3 (R=rare-earth element) exhibit three kinds of phase transitions with decreasing temperature: a structural transition from a pseudo-cubic to a monoclinic phase, a metal- insulator transition (MIT), and a magnetic transition from a paramagnetic state to an ordered one. The first two occur at the same temperature, which has led to a consensus that the MIT is driven by lattice distortions. We show here that the primary driving force for the MIT is magnetic; however because of the unusual d7 configuration of Ni, additional flexibility in spin configurations are also needed which symmetry-lowing structural deformations make possible. The latter enable Ni to disproportionate into two kinds: a high-spin and a low-spin configuration, which allow the system to reduce its unfavorable orbital moment and also open a gap.
format Preprint
id arxiv_https___arxiv_org_abs_2511_14960
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Origin of metal-insulator transition in rare-earth Nickelates
Acharya, Swagata
Tellekamp, Brooks
Jackson, Jerome
Pashov, Dimitar
Blackburn, Jeffrey L.
Alberi, Kirstin
van Schilfgaarde, Mark
Strongly Correlated Electrons
Materials Science
Superconductivity
Rare-earth nickelates RNiO3 (R=rare-earth element) exhibit three kinds of phase transitions with decreasing temperature: a structural transition from a pseudo-cubic to a monoclinic phase, a metal- insulator transition (MIT), and a magnetic transition from a paramagnetic state to an ordered one. The first two occur at the same temperature, which has led to a consensus that the MIT is driven by lattice distortions. We show here that the primary driving force for the MIT is magnetic; however because of the unusual d7 configuration of Ni, additional flexibility in spin configurations are also needed which symmetry-lowing structural deformations make possible. The latter enable Ni to disproportionate into two kinds: a high-spin and a low-spin configuration, which allow the system to reduce its unfavorable orbital moment and also open a gap.
title Origin of metal-insulator transition in rare-earth Nickelates
topic Strongly Correlated Electrons
Materials Science
Superconductivity
url https://arxiv.org/abs/2511.14960