Abstract
Phase transitions and equations of state of the alkaline earth fluorides , , and were examined by static compression to pressures as high as 146 GPa. Angle-dispersive x-ray diffraction experiments were performed on polycrystalline samples in the laser-heated diamond-anvil cell. We confirmed that at pressures less than 10 GPa all three materials undergo a phase transition from the cubic fluorite structure to the orthorhombic cotunnite-type structure. This work has characterized an additional phase transition in and : these materials were observed to transform to a hexagonal -type structure between 63–79 GPa and 28–29 GPa, respectively, upon laser heating. For , the -type phase was confirmed by Rietveld refinement. Volumes were determined as a function of pressure for all high-pressure phases and fit to the third-order Birch-Murnaghan equation of state. For and , the fluorite-cotunnite transition results in a volume decrease of , while the bulk modulus of the cotunnite-type phase is the same or less than that of the fluorite phase within uncertainty. For all three fluorides, the volume reduction associated with the further transition to the -type phase is . The percentage increase in the bulk modulus across the transition is greater when the cation is smaller. While for , is , values for and are and . Although shock data for have been interpreted to show a transition to a highly incompressible phase above 100 GPa, this is not consistent with our static equation of state data.
5 More- Received 11 March 2010
DOI:https://doi.org/10.1103/PhysRevB.81.174121
©2010 American Physical Society