PreprintCC BY 4.0arXiv
Positive Temperature Coefficient of Anisotropy due to d6L Groundstate in ε-Fe2O3
Abstract
Positive anisotropy temperature coefficients (dK/dT>0) usually arise from hybridization between magnetic 3d states and strongly spin-orbit-coupled (SOC) subsystems. Yet ε-Fe2O3 shows dK/dT>0 (125-200~K) without an obvious SOC partner. We study pure and Cr-doped (with weakened Fe-O hybridization) ε-Fe2O3 across the transition from low temperature incommensurate to high-anisotropy magnetic phases. We identify a d6L groundstate in ε-Fe2O3 while reduced hybridization yields d6 + d6L2 in the Cr-doped system, highlighting metal-ligand hybridization as a route to tune magnetic, electronic and orbitronic properties.
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BibTeX
@misc{nickel2026positive,
title = {{Positive Temperature Coefficient of Anisotropy due to $d^6L$ Groundstate in $ε$-Fe$_2$O$_3$}},
author = {Rachel Nickel and Kurt Kummer and Johan van Lierop},
howpublished = {arXiv},
year = {2026},
month = sep,
doi = {10.48550/arxiv.2609.08927},
eprint = {2609.08927},
archivePrefix = {arXiv},
url = {https://arxiv.org/abs/2609.08927},
note = {CC BY 4.0},
}
RIS
TY - UNPB
TI - Positive Temperature Coefficient of Anisotropy due to d^6L Groundstate in ε-Fe_2O_3
AU - Rachel Nickel
AU - Kurt Kummer
AU - Johan van Lierop
PY - 2026
DA - 2026/09/08
PB - arXiv
DO - 10.48550/arxiv.2609.08927
UR - https://arxiv.org/abs/2609.08927
AB - Positive anisotropy temperature coefficients (dK/dT>0) usually arise from hybridization between magnetic 3d states and strongly spin-orbit-coupled (SOC) subsystems. Yet ε-Fe_2O_3 shows dK/dT>0 (125-200~K) without an obvious SOC partner. We study pure and Cr-doped (with weakened Fe-O hybridization) ε-Fe_2O_3 across the transition from low temperature incommensurate to high-anisotropy magnetic phases. We identify a d^6L groundstate in ε-Fe_2O_3 while reduced hybridization yields d^6 + d^6L^2 in the Cr-doped system, highlighting metal-ligand hybridization as a route to tune magnetic, electronic and orbitronic properties.
ER -