Abstract
The fine structure of the oxygen P3 ground state is computed using a rather simple multiconfiguration wave function. The approach is similar to that used in previously reported fine-structure calculations for the lowest nitrogen D2 and P2 states, and similar results are obtained, accounting for about 80% of the difference between the Hartree-Fock result for the spin-orbit coupling parameter and the value indicated by experiment. The contribution due to spin-spin coupling is also considered.

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