We have applied the M\"ossbauer effect to study the local atomic environments in metastable crystalline Fe100?(hyx{B}ₓalloys (1≤x≤12) produced by rapid quenching from the melt. For concentrations up to 9 at. % B, the spectra revealed the existence of three distinct⁵⁷Fe$ sites, characterized by room-temperature hyperfine fields of 330, 267, and 236 kOe, the first of which is that of Fe in bcc {α}-Fe. The other two sites were populated in the ratio 1:2, while the total amount of Fe atoms in them was nearly three times the number of B atoms present in the alloys. Furthermore, the temperature dependences of the hyperfine fields at these two sites were the same, although distinctly different from that of the {α}-Fe site. The M\"ossbauer results presented here, together with a nuclear-magnetic-resonance investigation previously reported, demonstrate that these alloys are not random solid solutions. Instead, they indicate that the alloys consist of a dispersion of very small regions, which have an orthorhombic-Fe₃B-like structure, embedded in an {α}-Fe matrix.
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Sánchez et al. (1986) studied this question.
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