“…This works reasonably well in those cases where the core-polarization contribution, B core , to the total hyperfine magnetic field, B hf , dominates over other contributions, as, for instance, the contribution from spin-polarized conduction electrons, B ce , (spin-polarized by magnetic atoms). As an example, let us consider the chemically ordered quasi-Heusler compound Fe 3 Si with the D0 3 structure, where two inequivalent Fe lattice sites exist [23,24]: Fe(D) sites with B hf (D) = 30.8 T and Fe(A) sites with B hf (A) = 20 T, and corresponding Fe atomic moments of μ Fe (D) = 2.2 μ B and μ Fe (A) = 1.35 μ B , as determined by magnetic neutron scattering [32]. This results in a ratio of 14.0 T/μ B for the D site and 14.8 T/μ B for the A site, i.e., in a deviation of ∼6%.…”