Orbital-dominated hyperfine fields and intermediate-valence behavior of Ce impurities in antiferromagnetic and
Phys. Rev. B 114, 024413 – Published 10 July, 2026
DOI: https://doi.org/10.1103/zj2v-5pf6
Abstract
A combined experimental and first-principles investigation of the magnetic hyperfine field at dilute Ce impurities in the antiferromagnetic intermetallics and is reported here. Perturbed angular correlation spectroscopy using probes reveals strongly reduced hyperfine fields of in both hosts, which are substantially smaller than the free-ion value and even reduced relative to . To elucidate the local origin of this suppression, we perform spin-polarized density functional calculations including spin-orbit coupling within supercell models that explicitly account for the antiferromagnetic order. A systematic comparison of local spin-density approximation (LSDA), , and hybrid B3PW91 functionals demonstrates that the hyperfine field at the Ce site is overwhelmingly dominated by the orbital contribution associated with the shell, while spin-dipolar and Fermi-contact terms nearly cancel out. Conventional (DFT being density functional approximation) artificially localizes the Ce states and strongly overestimates hyperfine field. In contrast, calculations with a hybrid functional with enhanced exact exchange reveal a resonance-like spectral weight at the Fermi level, yielding nearly quenched spin moments and hyperfine fields in excellent agreement with the experiment. Analysis of the electronic structure and charge-density redistribution indicates that the reduced lattice volume (from lanthanide contraction) of the and hosts exerts an effective chemical pressure on the Ce impurity comparable to the critical pressure of , thereby driving the Ce electrons into an intermediate-valence regime. These results establish hyperfine interactions as a sensitive microscopic probe of hybridization and demonstrate the importance of beyond-semilocal exchange-correlation functionals for reliable predictions of hyperfine properties in correlated rare-earth materials.