High Pressure Phase Transitions in FeO from Density Functional Theory, Quantum Monte Carlo and Dynamical Mean Field Theory
ORAL
Abstract
FeO has a rich behavior under pressure, exhibiting a structural phase transition as well as an insulator-metal transition and a spin collapse. The electronic transitions have been particularly difficult to explain because of the failure of Density Functional Theory (DFT) to capture the electronic state of FeO. We present results from three different methods to better understand the nature of this material. First, from DFT calculations we explore competing explanations for the spin collapse, finding that the increase in bandwidth is at least as important as the crystal field splitting. Additionally, we find that the ligand field effects are responsible for the majority of the change in the local energy levels on the Fe rather than the electrostatic crystal field effect. Secondly, we have performed Dynamical Mean Field Theory (DMFT) calculations. From these we find that the metal insulator transition involves the reorganization of the existing bands and not the appearance of new states at the Fermi level. Finally we test the validity of the approximate results obtained by DFT and DMFT by performing highly accurate Diffusion Monte Carlo calculations.
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Authors
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Luke Shulenburger
Geophysical Laboratory, Carnegie Institution
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Ken Esler
Geophysical Laboratory, Carnegie Institution
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Sergey Savrasov
University of California, Davis, Department of Physics, University of California, Davis, Department of Physics, University of California, Davis, California 95616, USA, UC Davis
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Jeongnim Kim
University of Illinois at Urbana-Champaign, NCSA, University of Illinois at Urbana-Champaign
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R.E. Cohen
Geophysical Laboratory, Carnegie Institiution, Geophysical Laboratory, Carnegie Institution, Geophysical Laboratory, Carnegie Institution of Washington