High-pressure phase transformations, pressure-induced amorphization, and polyamorphic transition of the clathrateRb 6.15 Si 46
Author(s) -
Denis Machon,
P. Toulemonde,
Paul F. McMillan,
M. Amboage,
Alfonso Muñoz,
P. RodríguezHernández,
A. San Miguel
Publication year - 2009
Publication title -
physical review b
Language(s) - English
Resource type - Journals
eISSN - 1538-4489
pISSN - 1098-0121
DOI - 10.1103/physrevb.79.184101
Subject(s) - clathrate hydrate , phase transition , bulk modulus , crystallography , raman spectroscopy , materials science , ab initio , diffraction , physics , amorphous solid , diamond anvil cell , thermodynamics , chemistry , hydrate , optics , organic chemistry , quantum mechanics
International audienceThe type-I clathrate Rb6.15Si46 with partly empty cage sites has been studied up to 36 GPa using Raman spectroscopy, synchrotron x-ray diffraction in diamond-anvil cells, and ab initio total-energy and lattice-dynamics calculations. A first phase transition is observed at 13±1 GPa and a "volume collapse" transition within the clathrate structure is then observed at 24±1 GPa. Pressure-induced amorphization into a high-density amorphous (HDA) state occurs above P=33±1 GPa. The HDA form transforms into a low-density amorphous polymorph during decompression. During the compression study using angle dispersive synchrotron x-ray diffraction techniques we measured bulk modulus parameters for rocksalt-structured TaO, included adventitiously in the clathrate sample [K0=293(3) GPa and K′0=5.4(3)]
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