The phase transition of AF2 difluorides strongly
depends
on pressure, temperature, and cationic radius. Here, we have investigated
the phase transition of three difluorides, including MgF2, CaF2, and BaF2, at simultaneously high pressures
and temperatures using Raman spectroscopy and X-ray diffraction in
externally heated diamond anvil cells up to 55 GPa at 300–700
K. Rutile-type difluoride MgF2 with a small cationic radius
undergoes a transition to the CaCl2-type phase at 9.9(1)
GPa and 300 K, to the HP-PdF2-type phase at 21.0(2) GPa,
and to the cotunnite-type phase at 44.2(2) GPa. The phase transition
pressure to the HP-PdF2 and cotunnite structure at 300
K for our single crystal was found to be higher than that in previous
studies using polycrystalline samples. Elevating the temperature increases
the transition pressure from rutile- to the CaCl2-type
phase but has a negative influence on the transition pressure when
MgF2 transforms from the HP-PdF2- to cotunnite-type
phase. Meanwhile, the transition pressure from the CaCl2- to HP-PdF2-type phase for MgF2 was identified
to be independent of the temperature. Raman peaks suspected to belong
to the α-PbO2-type phase were observed at 14.6–21.0(1)
GPa and 400–700 K. At 300 K, difluorides CaF2 and
BaF2 in the fluorite structure with larger cationic radii
transform to the cotunnite-type phase at 9.6(3) and 3.0(3) GPa at
300 K, respectively, and BaF2 further undergoes a transition
to the Ni2In-type phase at 15.5(4) GPa. For both CaF2 and BaF2, elevating the temperature leads to a
lower transition pressure from fluorite- to the cotunnite-type phase
but has little influence on the transition to the Ni2In
structure. Raman data provide valuable insights for mode Grüneisen
parameters. We note that the mode Grüneisen parameters for
both difluorides and dioxides vary linearly with the cation radius.
Further calculations for the mode Grüneisen parameters at high
pressures for MgF2, CaF2, and BaF2 yield a deeper understanding of the thermodynamic properties of
the difluorides.