Abstract
Iron pentacarbonyl has been thermally decomposed in an organic liquid. Mössbauer spectroscopy and x-ray diffraction studies show that the sample contains small particles of a metallic glass. Annealing of the particles at 523 K results in crystallization of the particles into a mixture of α-Fe and χ-. The mechanism of glass formation is discussed.
- Received 18 March 1985
DOI:https://doi.org/10.1103/PhysRevLett.55.410
©1985 American Physical Society