Origin of the Tetragonal-to-Orthorhombic Phase Transition in FeSe: A Combined Thermodynamic and NMR Study of Nematicity
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Abstract
The nature of the tetragonal-to-orthorhombic structural transition at T[s]≈90 K in single crystalline FeSe is studied using shear-modulus, heat-capacity, magnetization, and nuclear magnetic resonance measurements. The transition is shown to be accompanied by a large shear-modulus softening, which is practically identical to that of underdoped Ba(Fe, Co)[2]A[s2], suggesting a very similar strength of the electron-lattice coupling. On the other hand, a spin-fluctuation contribution to the spin-lattice relaxation rate is only observed below T[s]. This indicates that the structural, or “nematic, ” phase transition in FeSe is not driven by magnetic fluctuations.
Journal
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- Physical Review Letters
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Physical Review Letters 114 (2), 027001-, 2015-01-15
American Physical Society (APS)
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Details 詳細情報について
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- CRID
- 1050845760738340608
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- NII Article ID
- 120005555484
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- NII Book ID
- AA00773679
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- ISSN
- 00319007
- 10797114
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- HANDLE
- 2433/196040
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- Text Lang
- en
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- Article Type
- journal article
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- Data Source
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- IRDB
- Crossref
- CiNii Articles
- KAKEN