Pressure-Induced Amorphization and Phase Transformations in -LiAlSiO4
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his work presents a comprehensive study on pressure-induced amorphization (PIA) in -eucryptite(LiAlSiO4) and on the equilibrium states of so-formed amorphous phase at elevated temperatures. Ourresults revealed that at 300 K -LiAlSiO4 underwent progressive amorphization at pressures above 4.5GPa and became completely amorphous above 17.0 GPa. After release of pressure, -LiAlSiO4 that waspartially amorphized at 7.5, 14.0, and 16.0 GPa reverted back to its original crystalline state. Whensubjected to a complete loss of long-range structural order, the system was recovered as an amorphousstate and did not retain the so-called structural memory. Upon heating at high pressures, the partially orcompletely amorphous -LiAlSiO4 transformed into various crystalline phases at temperatures above973 K: between 6.9 and 10.7 GPa it was decomposed into a mixture of LiAlSi2O6 and LiAlO2; at 15.3GPa the two phases recombined to form a new phase with a spinel structure; and at 22 GPa the spinelphase of LiAlSiO4 was decomposed into its constituent oxides. The observed transformations are all ofa reconstructive type and also involve profound changes in atomic coordination environments. A largeactivation energy barrier associated with coordination changes and a hindrance of atomic mobility atkinetically low temperatures are the primary factors that trigger the PIA.

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