Positive Temperature Coefficient of Anisotropy due to Groundstate in -FeO
arXiv:2609.08927
Abstract
Positive anisotropy temperature coefficients () usually arise from hybridization between magnetic 3d states and strongly spin-orbit-coupled (SOC) subsystems. Yet -FeO shows (125-200~K) without an obvious SOC partner. We study pure and Cr-doped (with weakened Fe-O hybridization) -FeO across the transition from low temperature incommensurate to high-anisotropy magnetic phases. We identify a groundstate in -FeO while reduced hybridization yields in the Cr-doped system, highlighting metal-ligand hybridization as a route to tune magnetic, electronic and orbitronic properties.