Abstract
Investigations of electron spin resonance (ESR) spectra of Yb3+ and Dy3+ in the cubic crystal field of calcium oxide show g factors which are smaller than the calculated g factors. It is shown that covalent bonding through the effect of the orbital reduction factor can explain these discrepancies. It is found that (1k) is about 0.04, much smaller than found in the iron group, but larger than that found for rare earth ions in the crystal field of CaF2. From the ESR spectra of Dy3+ and Er3+ it is inferred that the fourth-order potential B4 is at least 200 times larger than the sixth-order potential B6.