Structure and order parameters in the pressure-induced continuous transition in TeO2

Abstract
Lattice parameters of TeO2 have been measured from 0 to 32.5 kbar by time-of-flight neutron diffraction. Atomic-position parameters have also been measured to 20 kbar for both the low-pressure tetragonal paratellurite phase and the high-pressure orthorhombic phase, which we determined to have a structure belonging to the D24(P212121) space group. We found no hysteresis in the lattice parameters or position parameters in cycling through the transition. We also found that (ba)2a02 in the high-pressure phase varied linearly with pressure with a slope of 2.53(1) × 104/kbar, going to zero at 9.1 kbar. We detected no discontinuity in volume or the c parameter, but observed anomalies in the slopes dVdP, d(a+b)dP, and dcdP. All of these observations are additional experimental evidence for the continuous nature of the transition. The observed D24 structure of the high-pressure phase is a subgroup of order 2 of the D44 paratellurite phase which means that the free energy is an even function of the order parameter, but third-order terms coupling the primary order parameter with secondary or induced order parameters can still be formed. These can be nonzero without affecting the second-order nature of the transition. The primary order parameter η1=e1e2 and the two induced order parameters which we observed, η2=e1+e2 and η3=e3, have been used to derive a Landau-like free-energy expansion describing the thermodynamics of the transition. Very little displacement of the Te atoms was observed in going through the transition, but the oxygen atoms underwent large displacements as a function of pressure. There is no change of size of the unit cell at the transition so it is a pure strain transition of the type first discussed by Anderson and Blount.