A simple procedure for estimating the wave-vector-dependent g shift of conduction electrons in sodium metal is described. The conduction-electron wave functions are approximated by single orthogonalized plane waves (SOPW), orthogonal to the $2p$, $2s$, and $1s$ ion-core wave functions. All the core wave functions are determined variationally in terms of a two-parameter ion-core potential. The binding energy and spin-orbit splitting of the $2p$ core state are adjusted to experimental values. It is found that the core functions have negligible amplitude at the boundary of the cellular polyhedron. The g shift is then approximately given by 2 times the expectation value of the orbital angular momentum in a unit cell, plus two small relativistic terms. The calculated Fermi-surface average of the g shift is -5×{}10^-4. Since the experimental values are (-6±{}2)×{}10^-4, (-8±{}2)×{}10^-4, and (-10±{}2)×{}10^-4, it is concluded that a large part of the g shift in sodium can be accounted for by using the SOPW method.
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Graaf et al. (1970) studied this question.
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