Why rare-earth ferromagnets are so rare: Insights from the p-wave Kondo model

Shadab Ahamed, Roderich Moessner, and Onur Erten
Phys. Rev. B 98, 054420 – Published 21 August 2018
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Abstract

Magnetic exchange in Kondo lattice systems is of the Ruderman-Kittel-Kasuya-Yosida type, whose sign depends on the Fermi wave vector kF. In the simplest setting, for small kF, the interaction is predominately ferromagnetic, whereas it turns more antiferromagnetic with growing kF. It is remarkable that even though kF varies vastly among the rare-earth systems, an overwhelming majority of lanthanide magnets are in fact antiferromagnets. To address this puzzle, we investigate the effects of a p-wave form factor for the Kondo coupling pertinent to nearly all rare-earth intermetallics. We show that this leads to interference effects which for small kF are destructive, greatly reducing the size of the RKKY interaction in the cases where ferromagnetism would otherwise be strongest. By contrast, for large kF, constructive interference can enhance antiferromagnetic exchange. Based on this, we propose a route for designing ferromagnetic rare-earth magnets.

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  • Received 24 September 2017
  • Revised 4 August 2018

DOI:https://doi.org/10.1103/PhysRevB.98.054420

©2018 American Physical Society

Physics Subject Headings (PhySH)

Condensed Matter, Materials & Applied Physics

Authors & Affiliations

Shadab Ahamed1,2, Roderich Moessner1, and Onur Erten1,3

  • 1Max-Planck-Institute for the Physics of Complex Systems, Dresden 01187, Germany
  • 2Department of Physics, Indian Institute of Science, Bangalore 560 012, India
  • 3Department of Physics, Arizona State University, Tempe, Arizona 85287, USA

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Issue

Vol. 98, Iss. 5 — 1 August 2018

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