An electron-paramagnetic-resonance study of rare-earth impurities in II-VI compounds has been made. Isolated trivalent rare-earth ions are found to be substitutional for the metal ion in the zinc-blende crystals. Spectra from trivalent ions both at the isolated substitutional site and incorporated in additional unknown ways are observed in the wurtzite crystals. Shifts in the g factor are noted to depend on host covalency in the case of isolated substitutional Yb³⁺. Yb³⁺-(noblemetal)¹⁺ associates are studied in CdTe. Observation of ligand hyperfine structure shows that, in this instance, the rare earth is interstitial. Generally, the results indicate that the point-charge model may be usefully applied to determine the mechanism of rare-earth incorporation in II-VI compounds from observation of their paramagnetic-resonance spectra.
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Watts et al. (1968) studied this question.
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