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Phys. Rev. B 76, 212101 (2007) [4 pages]

Symmetry lowering under high pressure: Structural evidence for f-shell delocalization in heavy rare earth metal terbium

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Nicholas C. Cunningham1, Wei Qiu1, Kevin M. Hope2, Hanns-Peter Liermann3, and Yogesh K. Vohra1
1Department of Physics, University of Alabama at Birmingham (UAB), Birmingham, Alabama 35294-1170, USA
2Department of Biology, Chemistry and Mathematics, University of Montevallo, Montevallo, Alabama 35115, USA
3High Pressure Collaboration Access Team (HPCAT) and Geophysical Laboratory, Advanced Photon Source, Argonne National Laboratory, Argonne, Illinois 60439, USA

Received 11 July 2007; revised 19 August 2007; published 10 December 2007

Heavy rare earth metal terbium has been studied at synchrotron sources using both angular and energy dispersive x-ray diffraction to a maximum pressure of 155 GPa (volume fraction VV0=0.39). The complete regular trivalent rare earth structural sequence, hcp→α-Sm→double hcp→fcc→distorted fcc (hR24), is observed at low pressures except for the undistorted fcc. At 51±2 GPa, terbium undergoes a 5% volume collapse transitioning to C2∕m monoclinic. The open, low symmetry structure is reminiscent of the 4f delocalization phenomenon in the light rare earth metals, particularly the α phase of cerium.

© 2007 The American Physical Society

URL:
http://link.aps.org/doi/10.1103/PhysRevB.76.212101
DOI:
10.1103/PhysRevB.76.212101
PACS:
62.50.+p, 64.70.Kb, 64.30.+t, 71.20.Eh