Crossing N=28 Toward the Neutron Drip Line: First Measurement of Half-Lives at FRIB

H. L. Crawford, V. Tripathi, J. M. Allmond, B. P. Crider, R. Grzywacz, S. N. Liddick, A. Andalib, E. Argo, C. Benetti, S. Bhattacharya, C. M. Campbell, M. P. Carpenter, J. Chan, A. Chester, J. Christie, B. R. Clark, I. Cox, A. A. Doetsch, J. Dopfer, J. G. DuarteP. Fallon, A. Frotscher, T. Gaballah, T. J. Gray, J. T. Harke, J. Heideman, H. Heugen, R. Jain, T. T. King, N. Kitamura, K. Kolos, F. G. Kondev, A. Laminack, B. Longfellow, R. S. Lubna, S. Luitel, M. Madurga, R. Mahajan, M. J. Mogannam, C. Morse, S. Neupane, A. Nowicki, T. H. Ogunbeku, W. J. Ong, C. Porzio, C. J. Prokop, B. C. Rasco, E. K. Ronning, E. Rubino, T. J. Ruland, K. P. Rykaczewski, L. Schaedig, D. Seweryniak, K. Siegl, M. Singh, S. L. Tabor, T. L. Tang, T. Wheeler, J. A. Winger, Z. Xu

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Abstract

New half-lives for exotic isotopes approaching the neutron drip-line in the vicinity of N∼28 for Z=12-15 were measured at the Facility for Rare Isotope Beams (FRIB) with the FRIB decay station initiator. The first experimental results are compared to the latest quasiparticle random phase approximation and shell-model calculations. Overall, the measured half-lives are consistent with the available theoretical descriptions and suggest a well-developed region of deformation below Ca48 in the N=28 isotones. The erosion of the Z=14 subshell closure in Si is experimentally confirmed at N=28, and a reduction in the Mg38 half-life is observed as compared with its isotopic neighbors, which does not seem to be predicted well based on the decay energy and deformation trends. This highlights the need for both additional data in this very exotic region, and for more advanced theoretical efforts.

Original languageEnglish
Article number212501
JournalPhysical Review Letters
Volume129
Issue number21
DOIs
StatePublished - Nov 18 2022

Funding

We would like to thank the entire operations team at FRIB for their amazing work in beam delivery during the experiment, and for all of the work leading up to this measurement. This material is based upon work supported in part by the U.S. Department of Energy, Office of Science, Office of Nuclear Physics under Contracts No. DE-AC02-06CH11357 (ANL), No. DE-AC02-98CH10946 (BNL), No. DE-AC02-05CH11231 (LBNL), No. DE-AC52-07NA27344 (LLNL), No. DE-SC0020451 (Michigan State), No. DE-SC0014448 (Mississipi State), No. DE-AC05-00OR22725 (ORNL), and No. DE-FG02-96ER40983 (UTK). This work was also supported by the U.S. National Science Foundation under Grants No. PHY-2012522 (FSU) and No. PHY-1848177 (CAREER) (Mississippi State). The research was also sponsored by the U.S. Department of Energy, National Nuclear Security Administration under Award No. DE-NA0003180 (Michigan State) and the Stewardship Science Academic Alliances program through DOE Awards No. DE-NA0003899 (UTK) and No. DOE-DE-NA0003906 (Michigan State), and NSF Major Research Instrumentation Program Award No. 1919735 (UTK).

FundersFunder number
National Science FoundationPHY-2012522, 1919735
U.S. Department of Energy
Office of Science
National Nuclear Security AdministrationDE-NA0003180, DE-NA0003899, DOE-DE-NA0003906
Nuclear PhysicsDE-AC02-06CH11357
Argonne National LaboratoryDE-AC02-05CH11231, DE-AC02-98CH10946
Lawrence Livermore National LaboratoryDE-SC0020451, DE-AC05-00OR22725, DE-SC0014448
Oak Ridge National LaboratoryDE-FG02-96ER40983
Lawrence Berkeley National LaboratoryDE-AC52-07NA27344
Florida State UniversityPHY-1848177

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