A detailed investigation of the temperature- and pressure-dependent local and long-range structure of BiVO₄, one of the most extensively studied materials in contemporary materials science is presented.1, 2 BiVO₄ is a promising photocatalyst for water splitting due to its favourable band gap, high chemical stability, and suitable band-edge positions, and has also been explored as a microwave dielectric material.
BiVO₄ undergoes a reversible second-order ferroelastic phase transition at ~528 K from the monoclinic fergusonite structure (mf-BiVO₄) to the tetragonal scheelite structure (ts-BiVO₄), driven by a q ≈ 0 soft optical Bg phonon mode. An analogous transition occurs under pressure at ~1.5 GPa. This transition involves changes in the distortion of the BiO₈ and VO₄ polyhedra, with the Bi–O bond environments evolving from four distinct bond lengths to two, and the V–O bonds from two distinct lengths to one.
DFT studies show that the Bi 6s² lone pair electrons and V⁵⁺ d⁰ cations enhances orbital hybridisation, reducing the band gap and enabling visible-light absorption with a conduction band edge near the thermodynamic H₂ evolution potential.3 Conventional DFT approaches struggle to reproduce the experimentally observed room-temperature mf structure, with the PBE functional predicting the high-symmetry ts phase to be energetically favoured.4 This is consistent with predictions from the Bastide phase diagram for ABX₄ compounds based on ionic radii. The structural distortions distinguishing fergusonite from scheelite are comparatively subtle in BiVO₄ relative to other AIIIBVO₄ materials.
Despite its centrosymmetric structure, studies of BiVO₄ ceramics 5 and thin films6 have reported polar domains, polar domain walls, and phenomena including flexoelectricity, piezo-photocatalysis, and anomalous photovoltaic effects. These observations motivate a comprehensive structural re-examination. We employed variable-temperature and high-pressure X-ray and neutron scattering to probe both short- and long-range structural responses in BiVO₄ and to clarify the structural origins of these unexpected polar behaviours.