文摘
The structural phase transition of gadolinium鈥搒candium鈥揼allium garnet (Gd3Sc2Ga3O12, GSGG) has been studied at high pressure and high temperature using the synchrotron X-ray diffraction technique in a laser-heated diamond anvil cell. The GSGG garnet transformed to an orthorhombic perovskite structure at approximately 24 GPa after laser heating to 1500鈥?000 K. The garnet-to-perovskite phase transition is associated with an 8% volume reduction and an increase in the coordination number of the Ga3+ or Sc3+ ion. The orthorhombic perovskite GSGG has bulk modulus B0 = 194(15) GPa with B0鈥?= 5.3(8), exhibiting slightly less compression than the cubic garnet structure of GSGG with B0 = 157(15) GPa and B0鈥?= 6.5(10). Upon compression at room temperature, the cubic GSGG garnet became amorphous at 65 GPa. Coupled with the amorphous-to-perovskite phase transition in Y3Fe5O12 and Gd3Ga5O12 at high-pressure鈥搕emperature conditions, we conclude that amorphization should represent a new thermodynamic state resulting from hindrance of the garnet-to-perovskite phase transition, whereas the garnet-to-amorphous transition in rare-earth garnets should be kinetically hindered at room temperature.