Magnetism of metastable γ-Fe 85 Pd 15 nanowire arrays across an unusually broad temperature range (5 K to 800 K)
; Aprea, María Soledad
; Céspedes, Eva ; Martínez, José Luis ; Urreta, Silvia Elena ; Vázquez, Manuel Otros responsables
Fecha
08/2024
Editorial
Royal Society of Chemistry
Revista
Nanoscale
Título del libro
Nombre del evento
Fecha del evento
Institución organizadora
ISSN
2040-3364
eISSN
ISBN
Idioma
Inglés
Tipo del evento
Clasificación temática
Palabras clave
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 T0 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.
Colecciones
Aprobación
Revisión
Complementado por
Referenciado por
Licencia Creative Commons
Excepto donde se indique lo contrario, la licencia de este ítem se describe como by-nc-sa
