Abstract
We report a sequence of continuous phase transformations in iron telluride, FeTe with , which is observed by combining neutron diffraction, magnetic susceptibility, and specific-heat measurements on single-crystal samples. While a gradual increase of magnetic scattering near the wave vector is seen below K, a temperature where the discontinuous first-order magnetostructural phase transition is found in systems with small (), the reduction of the lattice symmetry in FeTe only occurs at K. Below K, the long-range magnetic order develops, the incommensurate wave vector of which varies with temperature. Finally, at K, the system enters the low- phase, where is locked at . We conclude that these instabilities are weak compared to the strength of the underlying interactions, and we suggest that the impact of the Fe interstitials on the transitions can be treated with random-field models.
- Received 1 September 2011
DOI:https://doi.org/10.1103/PhysRevB.85.085105
©2012 American Physical Society