Self-organized formation of exchange-spring magnets in Permalloy-derived epitaxial silicide nanostructures, fabricated by deposition of Ni80Fe20 onto a vicinal Si(111) substrate, is reported. The crystal structure of bar-shaped silicide nanostructures decorating Si(111) surface steps, following thermally activated reaction between Ni, Fe, and Si surface atoms, was identified as ternary β-Fe(Ni)Si2 phase, in well-defined (1¯11¯) Si || (2¯2¯0) β and [011] Si || [001] β orientation relations with the substrate. At the same time, chemical composition within the islands was Fe-rich and Fe-deficient in comparison with the original stoichiometric Permalloy (Ni80Fe20) and not uniform, with higher concentration of Ni at the island bottoms, close to the interface with Si(111), creating de facto “compositional interfaces” within the islands, though no physical interfaces could be detected in a high-resolution structural-crystallographic analysis by transmission electron microscopy. Analysis of temperature-dependent magnetization reversal loops revealed, that the thicker and magnetically soft top part of the islands and yet magnetically softer and thinner bottom part, were magnetically exchange-coupled via the above “virtual” interfaces. Micromagnetic simulations, consistent with exchange-spring magnet, had further corroborated this conclusion.
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