Structure and order parameters in the pressure-induced continuous transition in Te
- 1 September 1975
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review B
- Vol. 12 (5), 1899-1907
- https://doi.org/10.1103/physrevb.12.1899
Abstract
Lattice parameters of Te 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 space group. We found no hysteresis in the lattice parameters or position parameters in cycling through the transition. We also found that in the high-pressure phase varied linearly with pressure with a slope of 2.53(1) × /kbar, going to zero at 9.1 kbar. We detected no discontinuity in volume or the parameter, but observed anomalies in the slopes , , and . All of these observations are additional experimental evidence for the continuous nature of the transition. The observed structure of the high-pressure phase is a subgroup of order 2 of the 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 and the two induced order parameters which we observed, and , 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.
Keywords
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