Static and dynamical properties in the Pr-based filled skutterudite compound PrFe4P12 revealed by a P31-NMR study

K. Ishida, H. Murakawa, K. Kitagawa, Y. Ihara, H. Kotegawa, M. Yogi, Y. Kitaoka, Ben-Li Young, M. S. Rose, D. E. MacLaughlin, H. Sugawara, T. D. Matsuda, Y. Aoki, H. Sato, and H. Harima
Phys. Rev. B 71, 024424 – Published 27 January 2005

Abstract

P31-NMR studies have been carried out to investigate magnetic properties in the Pr-based filled skutterudite compound PrFe4P12. This compound shows an unusual phase transition at TA6.5K, which is now regarded as antiferroquadrupole (AFQ) ordering from neutron-diffraction experiments. Splitting of the P-NMR spectrum due to the appearance of two P sites with different hyperfine fields was observed below TA. From the field dependence, the splitting seems to disappear in zero magnetic field, indicating that the different hyperfine fields are not due to magnetic order, but to the appearance of two inequivalent P sites below TA. This is ascribed to the distortion of the P cage surrounding a Pr ion below TA, which is associated with the Pr orbital ordering. The nuclear spin-lattice relaxation rate (1T1) shows the typical behavior of Kondo systems, where onset of local-moment screening due to the coupling between conduction and localized Pr4f electrons is observed below 50K. Far above a critical field HA50kOe, the Korringa behavior T1T=const is observed below 2K in 100kOe. The Korringa value below 2K is one order of magnitude larger than that in LaFe4P12, which has no 4f electrons. Our NMR experiment shows that the heavy-fermion state is realized far above HA in PrFe4P12. The magnetic fluctuations in PrFe4P12 are discussed from a comparison with typical heavy-fermion compounds. In magnetic fields below HA, 1T1 shows a sharp decrease below TA, however, in smaller magnetic fields less than 10kOe, 1T1 stays constant far below TA with a relatively large value. The temperature and field dependence of 1T1 reveals the presence of low-energy spin fluctuations in the low-temperature and low-field region. These unusual magnetic fluctuations are considered to originate from the magnetic dynamics of Pr-nuclear spins since the fluctuating magnetic field 1.4Oe and frequency 3.5MHz are so small. The nuclear ordering temperature is estimated to be 0.08mK using the nuclear exchange fluctuations derived from the observed 1T1 of P. We show that PrFe4P12 is a quite unique compound in which nuclear magnetism can be detected by P NMR thanks to the nonmagnetic ground state of the Pr4f moments.

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  • Received 10 February 2004

DOI:https://doi.org/10.1103/PhysRevB.71.024424

©2005 American Physical Society

Authors & Affiliations

K. Ishida1, H. Murakawa1, K. Kitagawa1, Y. Ihara1, H. Kotegawa2, M. Yogi2, Y. Kitaoka2, Ben-Li Young3, M. S. Rose3, D. E. MacLaughlin3, H. Sugawara4, T. D. Matsuda4,*, Y. Aoki4, H. Sato4, and H. Harima5

  • 1Department of Physics, Graduate School of Science, Kyoto University, Kyoto 606-8502, Japan
  • 2Department of Physical Science, Graduate School of Engineering Science, Osaka University, Toyonaka, 560-8531, Japan
  • 3Department of Physics, University of California, Riverside, California 92521-0413, USA
  • 4Department of Physics, Graduate School of Science, Tokyo Metropolitan University, Minami-Ohsawa 1-1, Hachioji, Tokyo 192-0397, Japan
  • 5The Institute of Scientific and Industrial Research, Osaka University, Ibaraki, Osaka 567-0047, Japan

  • *Present address: Advanced Science Research Center, Japan Atomic Energy Research Institute, Tokai, Ibaraki 319-1195, Japan.

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Vol. 71, Iss. 2 — 1 January 2005

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