Abstract
Amorphous Fe-B solids have been made over a wide range of compositions, up to 90 at.% Fe. Magnetic ordering occurs at a percolation-like threshold of . Above , the ordering temperature () rises sharply and linearly with Fe content. The value of reaches a maximum at about and decreases at the Fe-rich side. There is no accompanying maximum in the average Fe moment, which increases monotonically with Fe concentration.
- Received 17 February 1981
DOI:https://doi.org/10.1103/PhysRevB.24.1556
©1981 American Physical Society