Abstract
Deviations from the Landé interval rule governing separations between the J multiplets of atomic terms are known to stem from term mixing by the spin–orbit interaction. A phenomenological interaction of the form HE = Σnλn(L·S)n with 1 ≤ n ≤ p can account for any such separations if p = 2S , one less than the multiplicity of the term. The general theory of effective operators is applied to the spin–orbit interaction for electron configurations of the form lN , and it is shown that, through pth order in the perturbation expansion of the spin–orbit Hamiltonian h = ηΣi1i·si , the above form for HE obtains where λn = ηΣm(η / F2)m−1λnm, n ≤ m ≤ p . Assuming hydrogenlike wavefunctions for f electrons, the λnm are shown to be constants depending only on the term being considered and the number of equivalent electrons N . Using η and F2 values given in the literature, the λn are calculated for the ground terms of the triply ionized rare earths. Values for the λn have been reported for Nd3+, Tb3+, Ho3+, and Er3+ in CaWO4 where the Stark‐split energy levels of the ground terms were analyzed by treating the λn and the crystal‐field parameters in HX = ΣkmBkmCkm as adjustable. The theoretical and experimental values for λ1, λ2 and λ3 agree to within 2.6%, 7.0%, and 23%, respectively. The calculation is then inverted and η and F2 values for the four ions are determined by requiring the theoretical λn parameters to equal those obtained empirically. The η and F2 values obtained in this manner differ from those reported by 2.3% and 5.1%, respectively. It is therefore feasible, through the use of the effective spin–orbit Hamiltonian HE , to determine η and F2 values for the ground configuration of an ion by considering the ground term alone.

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