Abstract
Ion channeling in ( single crystals (x≤0.05) along the [001] and [011] directions shows that a fraction of the Fe lies out of the (001) plane and therefore does not substitute exactly in the Cu site. Both the backscattered MeV-ion beam and characteristic x rays are measured to obtain this result, and a simple theoretical basis of this process is described.
- Received 5 March 1991
DOI:https://doi.org/10.1103/PhysRevB.44.6927
©1991 American Physical Society