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 = ΣkmBkm†Ckm 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.