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Letter: Impact of pear-shaped fission fragments on mass-asymmetric fission in actinides

dc.contributor.authorScamps, Guillaume
dc.contributor.authorSimenel, Cedric
dc.date.accessioned2020-02-10T23:59:18Z
dc.date.issued2018-12-27
dc.date.updated2019-11-25T07:31:42Z
dc.description.abstractNuclear fission of heavy (actinide) nuclei results predominantly in asymmetric mass splits1. Without quantum shell effects, which can give extra binding energy to their mass-asymmetric shapes, these nuclei would fission symmetrically. The strongest shell effects appear in spherical nuclei, such as the spherical ‘doubly magic’ (that is, both its atomic and neutron numbers are ‘magic’ numbers) nucleus 132Sn, which contains 50 protons and 82 neutrons. However, a systematic study of fission2 has shown that heavy fission fragments have atomic numbers distributed around Z = 52 to Z = 56, indicating that the strong shell effects in 132Sn are not the only factor affecting actinide fission. Reconciling the strong spherical shell effects at Z = 50 with the different Z values of fission fragments observed in nature has been a longstanding puzzle3. Here we show that the final mass asymmetry of the fragments is also determined by the extra stability provided by octupole (pear-shaped) deformations, which have been recently confirmed experimentally around 144Ba (Z = 56)4,5, one of very few nuclei with shell-stabilized octupole deformation6. Using a quantum many-body model of superfluid fission dynamics7, we find that heavy fission fragments are produced predominantly with 52 to 56 protons, which is associated with substantial octupole deformation acquired on the way to fission. These octupole shapes, which favour asymmetric fission, are induced by deformed shells at Z = 52 and Z = 56. By contrast, spherical magic nuclei are very resistant to octupole deformation, which hinders their production as fission fragments. These findings may explain surprising observations of asymmetric fission in nuclei lighter than lead.en_AU
dc.description.sponsorshipThis work has been supported by the Australian Research Council under grant number DP160101254.en_AU
dc.format.extent13 pagesen_AU
dc.format.mimetypeapplication/pdfen_AU
dc.identifier.issn0028-0836en_AU
dc.identifier.urihttp://hdl.handle.net/1885/201609
dc.language.isoen_AUen_AU
dc.provenancehttp://sherpa.ac.uk/romeo/issn/0028-0836/ Author can archive pre-print (ie pre-refereeing). On author's personal website, institutional repository and funder designated repository (Sherpa/Romeo as of 17/2/2020)
dc.publisherNature Publishing Groupen_AU
dc.relationhttp://purl.org/au-research/grants/arc/DP160101254en_AU
dc.rights© 2018 Springer Nature Limiteden_AU
dc.sourceNatureen_AU
dc.titleLetter: Impact of pear-shaped fission fragments on mass-asymmetric fission in actinidesen_AU
dc.typeJournal articleen_AU
dcterms.accessRightsOpen Access
dcterms.dateAccepted2018-10-31
local.bibliographicCitation.lastpage385en_AU
local.bibliographicCitation.startpage382en_AU
local.contributor.affiliationScamps, Guillaume, University of Tsukubaen_AU
local.contributor.affiliationSimenel, Cedric, College of Science, The Australian National Universityen_AU
local.contributor.authoruidSimenel, Cedric, u4787848en_AU
local.description.notesImported from ARIESen_AU
local.identifier.absfor020202 - Nuclear Physicsen_AU
local.identifier.absseo970102 - Expanding Knowledge in the Physical Sciencesen_AU
local.identifier.ariespublicationu3102795xPUB164en_AU
local.identifier.citationvolume564en_AU
local.identifier.doi10.1038/s41586-018-0780-0en_AU
local.identifier.essn1476-4687en_AU
local.identifier.scopusID2-s2.0-85058879443
local.publisher.urlhttps://www.nature.com/en_AU
local.type.statusSubmitted Versionen_AU

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