“…The phase transition sequence of difluorides at high pressures is strongly dependent on the cation radius. − ,,,, At 300 K, rutile-type difluorides such as MgF 2 with a small cation radius of 0.72 Å undergo a second-order transformation to the orthorhombic CaCl 2 -type structure ( Pnnm , Z = 2) at ∼9 GPa and then transforms to the cubic HP-PdF 2 -type structure ( Pa 3̅, Z = 4, also misidentified as a “pyrite-type” structure in some studies) at ∼14 GPa. ,, However, an additional α-PbO 2 -type phase was predicted by theoretical calculation to be stable between CaCl 2 - and HP-PdF 2 -type phases . Further elevating pressure to ∼38 GPa leads to the transition to the cotunnite-type structure ( Pnma , Z = 4). ,− Increasing the cation radius leads to a decrease in the phase transition pressure to CaCl 2 - and HP-PdF 2 -type structures. , For example, ZnF 2 with a cation radius of 0.74 Å transitions to the CaCl 2 -type phase at 4.5 GPa and to the HP-PdF 2 -type structure at 10 GPa, which are much lower than those of MgF 2 at 300 K. , Of particular interest is the rutile-type MnF 2 , which transforms to the ZrO 2 - or SrI 2 -type rather than CaCl 2 -type structure at ∼3 GPa. , In contrast to the HP-PdF 2 -type MgF 2 , which directly transitions into the cotunnite structure at higher pressures, some transition metal difluorides like ZnF 2 and CoF 2 will transform into the AgF 2 - or cubic fluorite-type structures before changing to the cotunnite structure. , …”