New isomeric transition in Mg36 : Bridging the N=20 and N=28 islands of inversion

Here, we observed a new isomeric γ transition at 168 keV in 36Mg, with a half-life of T1/2=90⁢($^{+410}_{-50}$) ns. We propose that the observed transition deexcites a new 0+ isomeric state at 833 keV and populates the previously known first 2+ state. The existence of this isomer is consistent with...

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Veröffentlicht in:Physical review. C 2024-06, Vol.109 (6)
Hauptverfasser: Madurga, M., Christie, J. M., Xu, Z., Grzywacz, R., Poves, A., King, T., Allmond, J. M., Chester, A., Cox, I., Farr, J., Fletcher, I., Heideman, J., Hoskins, D., Laminack, A., Liddick, S., Neupane, S., Richard, A. L., Shimizu, N., Shuai, P., Siegl, K., Utsuno, Y., Wagenknecht, P., Yokoyama, R.
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Sprache:eng
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Zusammenfassung:Here, we observed a new isomeric γ transition at 168 keV in 36Mg, with a half-life of T1/2=90⁢($^{+410}_{-50}$) ns. We propose that the observed transition deexcites a new 0+ isomeric state at 833 keV and populates the previously known first 2+ state. The existence of this isomer is consistent with the predictions of the large-scale shell-model calculations of 36Mg using the sdpf-u-mix interaction. The observed excitation energy of the second 0+ state is caused by the small energy separation between two prolate-deformed configurations where the intruder configuration corresponds to two-neutron excitations from the sd to the pf shell. Within this interpretation, 36Mg becomes the crossing point between nuclei in which ground state deformed/superdeformed configurations are caused by the dominance of N=20 intruders (32,34Mg) and nuclei where deformed configurations are associated with the breaking of the N=28 closure and a large occupancy of the 1⁢p3/2 neutron orbit (38Mg and beyond). We found the lack of three-body monopole corrections in other effective interactions results in a predominance of N=20 intruder configurations past 38Mg incompatible with our observation. We conclude that 36Mg bridges the N=20 and N=28 islands of inversion, forming the so-called big island of deformation.
ISSN:2469-9985
DOI:10.1103/physrevc.109.l061301