On the origin of asymmetric fission of actinides
Guillaume Scamps, C\'edric Simenel

TL;DR
This paper explains the asymmetric fission of actinide nuclei by showing that octupole (pear-shaped) deformations, stabilized by shell effects at Z=52-56, play a key role in determining the mass asymmetry of fission fragments.
Contribution
The study demonstrates that octupole deformations, stabilized by shell effects at Z=52-56, are crucial in understanding asymmetric fission, extending beyond the traditional focus on spherical shell closures.
Findings
Heavy fission fragments are mainly produced with Z=52-56.
Octupole deformations favor asymmetric fission.
Spherical magic nuclei resist octupole deformation, hindering their fission fragment formation.
Abstract
Nuclear fission of heavy (actinide) nuclei results predominantly in asymmetric mass-splits. Without quantum shells, which can give extra binding energy to these mass-asymmetric shapes, the nuclei would fission symmetrically. The strongest shell effects are in spherical nuclei, so naturally the spherical "doubly-magic" Sn nucleus ( protons), was expected to play a major role. However, a systematic study of fission has shown that the heavy fragments are distributed around to 56, indicating that Sn is not the only driver. Reconciling the strong spherical shell effects at with the different values of fission fragments observed in nature has been a longstanding puzzle. Here, we show that the final mass asymmetry of the fragments is also determined by the extra stability of octupole (pear-shaped) deformations which have been recently…
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Taxonomy
TopicsNuclear physics research studies · Nuclear Materials and Properties · Astronomical and nuclear sciences
