Abstract

A mutual relation between the effective spectroscopic factors of the doublet ground state implied by the magnetization at saturation and the low-temperature susceptibility is established. Useful tools for the comparison and consistency check of the outcome of the EPR experiment and the results of the magnetic measurements at low-temperature are developed. Numerical values of the effective spectroscopic factor implied by the magnetization at saturation are provided for instant reference. The presented findings may be of valuable assistance in rationalizing the physical implications of the powder sample EPR experiment.

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