Abstract
Measurements of the paramagnetic resonance spectrum of manganese and ferric ions at low temperatures yield the values for the cubic field splitting parameter a as 18.6×104 and 205×104 cm1 respectively. The sign of a is positive in both cases, indicating that the twofold degenerate level is lower than the fourfold degenerate level. This is in contrast with Bleaney and Trenam's results on ferric alums who find a negative a. For gadolinium in CaF2, the constant a=175×104 cm1 and is also positive.

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