Abstract
Nuclear magnetic resonance on oriented nuclei was carried out using a sample of dilute and in iron prepared by ion implantation of radioactive precursor Rb isotopes. For , the beta-ray asymmetry was utilized to measure the magnetic hyperfine interaction frequency, , which led to the magnetic hyperfine field, , by using the known nuclear -factor. The field shift of the resonant frequency, for , implies a Knight shift value, . The interaction frequency and the field shift of obtained via the gamma-ray detection confirmed the previously reported results. A ratio of the measured and values for both and gave rise to the hyperfine anomaly, , which can explain discrepancies in the values of YFe as determined by various experiments.
- Received 18 April 2004
DOI:https://doi.org/10.1103/PhysRevB.70.132405
©2004 American Physical Society