The high-temperature phase transition between the tetragonal (scheelite) and monoclinic (fergusonite) forms of yttrium tantalite (${\mathrm{YTaO}}_{4}$ ) has been studied using a combination of first-principles calculations and a Landau free-energy expansion. Calculations of the Gibbs free energies show that the monoclinic phase is stable at room temperature and transforms to the tetragonal phase at 1430 \ifmmode^\circ\else\textdegree\fi{}C, close to the experimental value of $1426\ifmmode\pm\else\textpm\fi{}7$ \ifmmode^\circ\else\textdegree\fi{}C. Analysis of the phonon modes as a function of temperature indicate that the transformation is driven by softening of transverse acoustic modes with symmetry ${E}_{u}$ in the Brillouin zone center rather than the Raman-active ${B}_{g}$ mode. Landau free-energy expansions demonstrate that the transition is second order and, based on the fitting to experimental and calculated lattice parameters, it is found that the transition is a proper rather than a pseudoproper type. Together these findings are consistent with the transition being ferroelastic.
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