Abstract
The M\ossbauer spectra of ${\mathrm{Fe}}^{2+}$ in KMg${\mathrm{F}}_{3}$ and CaO have been studied under different magnitudes of an external magnetic field, oriented along the [100] and [111] directions, and these spectra are analyzed on the basis of the theory developed in the preceding paper. From the semiexperimental values of the Ham reduction factors thus deduced, the nature of the vibronic coupling in these systems is inferred.
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