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Local magnetic moments in iron and nickel at ambient and Earth's core conditions.
Hausoel, A; Karolak, M; Sasιoglu, E; Lichtenstein, A; Held, K; Katanin, A; Toschi, A; Sangiovanni, G.
Affiliation
  • Hausoel A; Institut für Theoretische Physik und Astrophysik, Universität Würzburg, Am Hubland, D-97074 Würzburg, Germany.
  • Karolak M; Institut für Theoretische Physik und Astrophysik, Universität Würzburg, Am Hubland, D-97074 Würzburg, Germany.
  • Sasιoglu E; Peter Grünberg Institut and Institute for Advanced Simulation, Forschungszentrum Jülich and JARA, 52425 Jülich, Germany.
  • Lichtenstein A; Institut für Physik, Martin-Luther-Universität Halle-Wittenberg, 06120 Halle (Saale), Germany.
  • Held K; Institut für Theoretische Physik, Universität Hamburg, Jungiusstrasse 9, 20355 Hamburg, Germany.
  • Katanin A; Institute of Solid State Physics, TU Wien, 1040 Vienna, Austria.
  • Toschi A; M. N. Mikheev Institute of Metal Physics, 620990 Ekaterinburg, Russia.
  • Sangiovanni G; Ural Federal University, 620002 Ekaterinburg, Russia.
Nat Commun ; 8: 16062, 2017 07 12.
Article in En | MEDLINE | ID: mdl-28799538
ABSTRACT
Some Bravais lattices have a particular geometry that can slow down the motion of Bloch electrons by pre-localization due to the band-structure properties. Another known source of electronic localization in solids is the Coulomb repulsion in partially filled d or f orbitals, which leads to the formation of local magnetic moments. The combination of these two effects is usually considered of little relevance to strongly correlated materials. Here we show that it represents, instead, the underlying physical mechanism in two of the most important ferromagnets nickel and iron. In nickel, the van Hove singularity has an unexpected impact on the magnetism. As a result, the electron-electron scattering rate is linear in temperature, in violation of the conventional Landau theory of metals. This is true even at Earth's core pressures, at which iron is instead a good Fermi liquid. The importance of nickel in models of geomagnetism may have therefore to be reconsidered.