Pressure-Induced Concurrent Transformation to an Amorphous and Crystalline Phase in Berlinite-Type
- 1 December 1997
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review Letters
- Vol. 79 (22), 4409-4412
- https://doi.org/10.1103/physrevlett.79.4409
Abstract
X-ray diffraction, Raman scattering, and Mössbauer spectroscopy provide a diverse description of the high pressure behavior of berlinite-type . At a pressure of 2.5(5) GPa, a transformation to a coexisting new crystalline and amorphous phase is observed with about equal abundance. The phase is identified as a type, where and ions, respectively, are sixfold and fourfold coordinated. In the 6–25 GPa range and after decompression, the relative abundance of the and phases remains unchanged. These phenomena of concurrent amorphous and crystalline transformations at low hydrostatic pressure and stable abundance ratio over a large pressure range are unique in pressure-induced structural transformations of analogs.
Keywords
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