The solidification products of levitated Fe83B17 studied by high-energy x-ray diffraction
Detailed high-energy x-ray diffraction studies were performed to gain insight into the evolution of phase formation in undercooled Fe 83 B 17 and the mechanism for the stabilization of face-centered cubic (fcc) Fe in the presence of Fe 23 B 6 . Fe 83 B 17 solidifies directly into either the equilibrium Fe 2 B + Fe phases or the metastable Fe 23 B 6 + Fe phases. When formed, the metastable Fe 23 B 6 phase either rapidly transforms into the equilibrium Fe 2 B phase within the solidification plateau or can persist down to ambient temperature. Here, we detail these different solidification behaviors in a set of thermal cycles taken from one sample and demonstrate the absence of a direct correlation with cooling rate and thermal history. We show that the coherent growth of Fe 23 B 6 and fcc Fe suppresses the allotropic transition from fcc Fe to bcc Fe. The temperature evolution of the phase fractions and lattice parameters is also presented.