Thermal history-dependent characteristics in van der Waals ferromagnet FeGeTe (x ∼ 0.16)
APL Materials, ISSN: 2166-532X, Vol: 12, Issue: 8
2024
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Example: if you select the 1-year option for an article published in 2019 and a metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019. If you select the 3-year option for the same article published in 2019 and the metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019, 2018 and 2017.
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Article Description
We investigated the thermal-history dependence of physical properties in a quenched FeGeTe (x ∼ 0.16) single crystal by measuring magnetization (M), electrical resistivity (ρ), Seebeck coefficient (S), and thermal conductivity (κ) as a function of temperature (T). The results reveal anomalies in these physical quantities around various transition points: ferromagnetic (T ∼ 310-300 K), helimagnetic (T ∼ 275 K), charge ordering (T ∼ 165 K), spin-reorientation (T* ∼ 100-120 K), and a Fermi-liquid (FL) phase below T ∼ 35 K. Using power-law fitting, the M(T) analysis near T shows that Fe moments become primarily itinerant after thermal cycling. The ρ(T) results indicate inherent residual stresses in the crystal that alter with thermal cycling, influencing ferromagnetic domain formations within grain boundaries. The system exhibits a strongly correlated FL behavior at low temperatures, which ceases above T due to spin fluctuations. In the T-range of T* ≤ T ≤ T, ρ(T) and S(T) analyses suggest significant electronic band structure modifications with multiband effects. The κ(T) data indicate phonon-dominated heat transport in the crystal, with a phonon behavior influenced by inherent lattice strains following initial thermal cycles, as evidenced by the decreased phonon peak height at low temperatures. In addition, there is evidence of phonon localization and electron-phonon coupling at higher temperatures.
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