An investigation of the pressure induced phase transition from the scheelite phase(I41/a,Z = 4) to thefergusonite-like phase (I 2/a,Z = 4) and to the LaTaO4 phase (P 21/c,Z = 4) of LiYF4 is presented. Employing density functional theory (DFT) within the generalized gradientapproximation, the structures were relaxed for a pressure range of 0–20 GPa without imposedsymmetry. The influence of pressure on the lattice vibrational spectrum of the scheelite phase(I41/a,Z = 4) was evaluated using the direct approach, i.e. using force constants calculated from atomicdisplacements. This work tends to confirm the transformations . At 20 GPa, a P 21/c structure with a pentacoordinated lithium cation is found to be the moststable phase. This structure is compatible with a transition driven by aBg zone-centre soft optic mode linked to a soft acoustic mode along the [] direction as observed from the evolution of the phonon dispersion curves as a function ofpressure.
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