Abstract
The D-value of Mn2+ in CoCl2·2H2O has been obtained to be −0.13 cm−1 by Date and Motokawa. The large negative D value is reasonably explained by introducing an effective exchange interaction of general form between the Mn2+ and the ground Kramers doublet of Co2+, taking account of the crystal symmetry. It is shown that the interaction −2JxzsxSz −2JyzsySz is responsible for the negative D-parameter. The effective exchange interaction is derived from the nondiagonal exchange between Mn2+ and Co2+ with respect to the cobaltous orbits by projecting the exchange to the ground Kramers doublet.