Stability of the Gd Magnetic Moment to the 500 GPa Regime
Z. P. Yin, W. E. Pickett

TL;DR
This study investigates the stability of Gd's magnetic moment under extreme pressure up to 500 GPa, revealing significant stability and gradual 4f electron delocalization, challenging the notion of an abrupt transition.
Contribution
It provides the first detailed theoretical analysis of Gd's magnetic and electronic structure evolution at ultra-high pressures using the LDA+U method.
Findings
Magnetic moment remains stable up to 500 GPa
4f occupation increases with pressure due to band broadening
Delocalization occurs gradually over a wide pressure range
Abstract
The evolution of the magnetic moment and various features of the electronic structure of fcc Gd are followed to reduced volume V/Vo = 0.125 using the LDA+U correlated band method. The stability of the moment is substantial; crude estimates of this signature of a possible ``Mott transition'' in the 4f system suggest a critical pressure Pc 500 GPa. The occupation is found to increase under pressure due to broadening and lowering of the minority states. This trend is consistent with the interpretation of x-ray spectra of Maddox et al. across the volume collapse transition at 59 GPa, and tends to support their suggestion that the delocalization of the 4f states in Gd differs from the original abrupt picture, being instead a process that occurs over an extended range of pressure.
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Taxonomy
TopicsHigh-pressure geophysics and materials · Rare-earth and actinide compounds · Theoretical and Computational Physics
