Artículo

Magnetism of metastable γ-Fe 85 Pd 15 nanowire arrays across an unusually broad temperature range (5 K to 800 K)

Bercoff, Paula Gabriela Icon; Aprea, María Soledad Icon; Céspedes, Eva ; Martínez, José Luis ; Urreta, Silvia Elena ; Vázquez, Manuel

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Fecha

08/2024

Editorial

Royal Society of Chemistry

Revista

Nanoscale

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ISSN

2040-3364

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Inglés

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Clasificación temática

Resumen

Arrays of 50 nm diameter Fe85Pd15 cylindrical nanowires were electrochemically grown, crystallizing in a metastable γ-Fe(Pd) fcc A1 disordered solid solution. After performing a heating-cooling thermal cycle between 300K and 1000K, the γ-Fe(Pd) fcc metastable phase still predominates (97%), coexisting with a not-fully-identified minority phase. The thermal cycling induces a moderate increase in the crystallite size and a reduction of the lattice parameter although leading to a significant heating-cooling magnetic hysteresis. No further changes in temperature-dependent magnetization, M(T), are observed during subsequent cycling. The full-range (5K to 800K) saturation magnetization Ms(T) curve is quite accurately described by a phenomenological expression, which provides a Bloch-type contribution as T0 and undergoes the critical behavior 𝑀(𝑇) (𝑇𝐶 – 𝑇) 1 𝛽 near the Curie temperature TC. An upturn in Ms(T) is observed below 100 K which is described by a spin-glass-like second contribution, with freezing temperature Tf = (80 ± 2) K, and kBTf comparable to the exchange interactions in Fe-Pd systems. A Curie temperature of TC=830K, and a critical exponent value  = 0.42±0.05 are estimated. These regimes (below and above 100K) are also observed in the magnetization process. The temperature dependence of coercivity between 100K and 800K is consistent with a nucleation/propagation remagnetization mechanism, with activation energy of (320 ± 20) kJ mol-1 and critical field for magnetization reversal of (65 ± 1) mT, at 0K. The analysis of the effective magnetic anisotropy as a function of temperature allows us to conclude that it essentially arises from the balance between different magnetostatic contributions.

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