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    Shell effects in quasifission toward Hg180: Insights into fission asymmetric modes

    Yingge Huang (黄英格)1,2, Haozhao Liang (梁豪兆)2,3,4,*, and Jun Su (苏军)1,5,†

    • *Contact author: haozhao.liang@phys.s.u-tokyo.ac.jp
    • †Contact author: sujun3@mail.sysu.edu.cn

    Phys. Rev. C 114, 014618 – Published 14 July, 2026

    DOI: https://doi.org/10.1103/qdgj-bqbz

    Abstract

    Background: The experiment of Hg180 fission revealed a possible “new asymmetric fission mode” in the preactinide region, posing challenges to current fission theory. Similarity in shell effects is observed between fission and quasifission, providing the possibility for widely exploring the topography of a fission potential-energy surface (PES).

    Purpose: We aim to investigate the shell effects in the quasifission toward Hg180 and to explore their connection with the Hg180 fission.

    Method: Zn68+Sn112, Se74+Pd106, Kr80+Ru100, and Kr84+Ru96 central collisions at different energies and projectile orientations are calculated using the Skyrme time-dependent Hartree-Fock approach. The static fission properties are calculated with the constrained Hartree-Fock-Bogoliubov method and compared with the quasifission results.

    Results: Shell effects are found to hinder mass equilibration between the prefragments, enhancing the production of fragments near the 80/100 mass split. By comparing the quasifission trajectories with the PES in the (Q20,Q30) space, the role of the PES ridge in forming fragments is identified. The presence of the asymmetric valley causes the Zn68+Sn112 quasifission to exhibit a prefragment mass equilibration process and scission-point configuration similar to those of Hg180 fission. The elongated light fragment is found to be a key factor in reproducing the experimental fission total kinetic energies. Meanwhile, a more pronounced proton shell gap is found in the Zn68+Sn112 quasifission compared with other reactions.

    Conclusions: By using quasifission dynamics as a probe of the fission pathway, the present calculations help clarify the specific influence of the PES topography and provide support for the dominance of proton shell effects and light fragment deformation in preactinide fission.

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