Abstract
Trivalent lead impurity ions have been detected by electron-spin resonance (ESR) to occur in diamagnetic garnet crystals of which were grown from a PbO-Pb based flux. From the observed weak anisotropy of the hyperfine interaction, it could be positively established that the ions occupy the dodecahedral sites in the garnet lattice. Trivalent lead impurity ions were also found to occur in the other diamagnetic garnet hosts, , , and .
- Received 16 February 1973
DOI:https://doi.org/10.1103/PhysRevB.8.1
©1973 American Physical Society