Electronic and structural properties of rare earth metals at normal and high pressures: Eu and Yb

1986 ◽  
Vol 59 (3-4) ◽  
pp. 277-286 ◽  
Author(s):  
B.I. Min ◽  
H.J.F. Jansen ◽  
T. Oguchi ◽  
A.J. Freeman
Science ◽  
1964 ◽  
Vol 144 (3614) ◽  
pp. 69-71 ◽  
Author(s):  
G. J. Piermarini ◽  
C. E. Weir

2014 ◽  
Vol 90 (16) ◽  
Author(s):  
O. B. Tsiok ◽  
L. G. Khvostantsev ◽  
A. V. Golubkov ◽  
I. A. Smirnov ◽  
V. V. Brazhkin

1997 ◽  
Vol 499 ◽  
Author(s):  
Steven Beaver ◽  
Gary N. Chesnut ◽  
Yogesh K. Vohra

ABSTRACTA high-pressure phase of gadolinium is completely described for the first time. This phase, HR24, is found to exist at 46 GPa. The structure is examined for evidence of delocalization of the f shell, and the evolution of the HR24 phase with increasing pressure is discussed.


2008 ◽  
Vol 1104 ◽  
Author(s):  
Yogesh K. Vohra ◽  
Bagvanth Reddy Sangala ◽  
Andrew K. Stemshorn ◽  
Kevin M. Hope

AbstractHigh-pressure studies have been performed on heavy rare earth metals Terbium (Tb) to 155 GPa and Holmium (Ho) to 134 GPa in a diamond anvil cell at room temperature. The following crystal structure sequence was observed in both metals hcp ⟶ Sm-type ⟶ dhcp ⟶ distorted fcc (hR-24) ⟶ monoclinic (C2/m) with increasing pressure. The last transformation to a low symmetry monoclinic phase is accompanied by a volume collapse of 5 % for Tb at 51 GPa and a volume collapse of 3 % for Ho at 103 GPa. This volume collapse under high pressure is reminiscent of f-shell delocalization in light rare earth metal Cerium (Ce), Praseodymium (Pr), and heavy actinide metals Americium (Am) and Curium (Cm). The orthorhombic Pnma phase that has been reported in Am and Cm after f-shell delocalization is not observed in heavy rare earth metals under high pressures.


1997 ◽  
Vol 04 (06) ◽  
pp. 1155-1160 ◽  
Author(s):  
R. FASEL ◽  
P. AEBI ◽  
L. SCHLAPBACH ◽  
T. GREBER ◽  
J. OSTERWALDER

A particularly interesting phenomenon of rare-earth metals and their compounds is the mixed valence, which is intimately connected with the structural properties of a material. We report structural and spectroscopic results from the [Formula: see text] interface, with particular emphasis on the interplay between surface structure and valence. A strong reconstruction of the substrate surface is observed, with the Yb atoms occupying substitutional sites. A small fraction of Yb atoms is identified to occupy second-layer sites in otherwise unreconstructed surface patches. It is shown that these subsurface Yb atoms are in a mixed-valent 4f14-δ state, whereas the surface atoms in the [Formula: see text] geometry persist in the divalent 4f14 state.


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