The crystal-field parameters calculated using a theory of OPW type developed in the previous paper have been compared with the values deduced from experiment for the heavy rare earth metals and two dilute alloy systems, Er: Mg and Er: Zr. Good agreement with experiment is obtained for A 0 2 < r 2 > for thulium metal, and also for the A 6 6 < r 6 > parameters in all cases where data is available. If a value for the f resonance parameter of -9.8 × 10 -2 is chosen, the correct g -values for Er: Mg are obtained. In the other cases considered agreement with experiment is less satisfactory but is nevertheless considerably better than point charge calculations.
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Dixon et al. (1971) studied this question.
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