Non-ionic contributions to the electric-field gradient at $^{181}$Ta and $^{111}$Cd impurity sites in R$_2$O$_3$ (R= Sc, In, Lu, Yb, Tm, Er, Y, Ho, Dy, Gd, Eu, Sm) bixbyites
Leonardo A. Errico (1), Mario Renter\'ia (1), An\'ibal G. Bibiloni, (1), Kristian Freitag, (2) ((1) Departamento de F\'isica, Facultad de, Ciencias Exactas, Universidad Nacional de La Plata, Argentina, (2) Helmholtz, - Institut f\"ur Strahlen- und Kernphysik (ISKP)

TL;DR
This study uses TDPAC and ab initio calculations to analyze electric-field gradients at impurity sites in bixbyite oxides, revealing significant nonionic contributions originating from p-state electron populations.
Contribution
It provides the first quantitative evidence that nonionic electronic effects dominate the EFG at impurity sites in bixbyite oxides, supported by experimental and ab initio results.
Findings
Nonionic contributions to EFG are dominant in these systems.
p-state electron populations significantly influence the EFG.
Experimental and theoretical results are in good agreement.
Abstract
The time-differential perturbed-angular-correlation (TDPAC) technique was applied to the study of the internal electric-field gradient (EFG) in Eu- and Ho-sesquioxides in their cubic bixbyite phases. The results, as well as previous characterizations of the EFG at Ta sites in oxides with the bixbyite structure, were compared to those obtained in experiments using Cd as probe, and to point-charge model and {\it ab initio} results calculations for the EFG tensor at impurity sites in binary oxides. These studies provide quantitative information about electronic processes and the structural relaxations induced by the presence of impurity probes in the host lattices, and confirm the existence of nonionic contributions to the EFG in these systems. Our FP-LAPW calculations show that this nonionic contribution to the EFG is the dominating one, and that it is originated in the…
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Taxonomy
TopicsHigh-pressure geophysics and materials · Atomic and Subatomic Physics Research · Geological and Geochemical Analysis
