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    Magnetic dipole moments adjacent to doubly magic nuclei in self-consistent mean-field theory with realistic spin-isospin and tensor forces

    H. Nakada1,2,* and H. Iwata3

    • 1Department of Physics, Graduate School of Science, Chiba University, Yayoi-cho 1-33, Inage, Chiba 263-8522, Japan
    • 2Research Center for Nuclear Physics, The University of Osaka, Mihogaoka 10-1, Ibaraki, Osaka 567-0047, Japan
    • 3Department of Physics, Graduate School of Science and Engineering, Chiba University, Yayoi-cho 1-33, Inage, Chiba 263-8522, Japan

    • *Contact author: nakada@faculty.chiba-u.jp

    Phys. Rev. C 113, 014315 – Published 16 January, 2026

    DOI: https://doi.org/10.1103/zqgm-3qmy

    Abstract

    Magnetic dipole (M1) moments in nuclei neighboring the doubly magic core are investigated by self-consistent mean-field (SCMF) approaches that allow for the breaking of time-reversal symmetry. By the SCMF calculations with the M3Y-P6 interaction, which keeps realistic spin-isospin and tensor channels, the M1 moments are well reproduced, particularly those in the nuclei adjacent to jj-closed magicity. The results are in better agreement with the data than those with the Gogny-D1S interaction, slightly better than those of UNEDF1 supplemented by a spin-isospin channel adjusted to the M1 moments themselves, and comparable to the shell-model results with the chiral effective-field-theory (χEFT) interaction. Analyses via quadrupole moments, occupation numbers, and the lowest-order perturbation theory elucidate the cooperative effects of quadrupole deformation and spin correlation on the displacement from the Schmidt values, which has been known in terms of the quenching of the spin matrix elements. It is shown that a significant portion of the spin correlation is carried by the spin-isospin and tensor channels in the effective interaction. However, while agreement is remarkable at Snm131, Sn133, and Pb209, discrepancies remain at the Z=odd nuclei Sb133, Ti207, and Bi209, as in the χEFT-based shell-model results.

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