Rotation of Unidirectional Charge Density Wave in ErTe3 in Response to Antisymmetric Strain Revealed by X-ray Diffraction
ORAL
Abstract
We observed via x-ray diffraction (XRD) that application of anisotropic strain to an ErTe3 crystal can rotate the primary in-plane (here, the a/c plane) charge density wave (CDW) wavevector by 90o. ErTe3 belongs to the rare-earth tritelluride family, RTe3 (R=La-Pr, Sm, Gd-Tm), which are quasi-2D materials comprising nearly-square Te nets that exhibit unidirectional incommensurate CDW states. These materials are a model system to explore open questions regarding CDW formation and its interrelation with superconductivity.
Although RTe3 is weakly orthorhombic and the primary CDW forms along the c-axis, Kohn anomalies are nevertheless observed at equivalent wavevectors in both in-plane directions, suggesting the material is ‘almost tetragonal’. Here, we demonstrate that the direction of the primary CDW can in fact be switched from the c to a-axis by applying anisotropic in-plane strain. We also performed complementary transport measurements that corroborate the XRD results. Additionally, our measurements reveal evidence for a domain structure at intermediate strain values. Present verification of the ability to strain tune the CDW orientation in this material makes it an ideal candidate to host a possible vestigial nematic phase.
Although RTe3 is weakly orthorhombic and the primary CDW forms along the c-axis, Kohn anomalies are nevertheless observed at equivalent wavevectors in both in-plane directions, suggesting the material is ‘almost tetragonal’. Here, we demonstrate that the direction of the primary CDW can in fact be switched from the c to a-axis by applying anisotropic in-plane strain. We also performed complementary transport measurements that corroborate the XRD results. Additionally, our measurements reveal evidence for a domain structure at intermediate strain values. Present verification of the ability to strain tune the CDW orientation in this material makes it an ideal candidate to host a possible vestigial nematic phase.
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Presenters
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Anisha G Singh
- Stanford University