Spontaneous strain due to ferroquadrupolar ordering in UCuSn
arXiv:cond-mat/0306591 · doi:10.1103/PhysRevB.68.144413
Abstract
The ternary uranium compound UCuSn with a hexagonal ZrPtAl-type structure shows a phase transition at 16 K. We reported previously that huge lattice-softening is accompanied by the phase transition, which originates from ferroquadrupolar ordering of the ground state non-Kramers doublet . A macroscopic strain, which is expected to emerge spontaneously, was not detected by powder X-ray diffraction in the temperature range between 4.2 and 300 K. To search the spontaneous strain, we have carried out thermal expansion measurements on a single-crystalline sample along the , and axes using a capacitance technique with the resolution of . In the present experiment, we found the spontaneous strain which couples to the ground state doublet . The effect of uniaxial pressure along the , and axes on the transition temperature is also discussed.
4 pages, 5 figures, submitted to Phys. Rev. B