Direct measurement of hexacontatetrapole, {\gamma} decay from Fe
T. Palazzo · A. J. Mitchell🇦🇺 · G. J. Lane🇦🇺 · A. E. Stuchbery🇦🇺 · B. A. Brown🇺🇸 · M. W. Reed🇺🇸 · A. Akber · B. J. Coombes🇦🇺 · J. T. H. Dowie🇦🇺 · T. K. Eriksen🇳🇴 · M. S. M. Gerathy🇦🇺 · T. Kibédi🇦🇺 · T. Tornyi🇭🇺 · M. O. de Vries
The only proposed observation of a discrete, hexacontatetrapole () transition in nature occurs from the T = 2.54(2)-minute decay of Fe. However, there are conflicting claims concerning its -decay branching ratio, and a rigorous interrogation of -ray sum contributions is lacking. Experiments performed at the Australian Heavy Ion Accelerator Facility were used to study the decay of Fe. For the first time, sum-coincidence contributions to the weak and decay branches have been firmly quantified using complementary experimental and computational methods. Agreement across the different approaches confirms the existence of the real transition; the branching ratio and transition rate have also been revised. Shell model calculations performed in the full model space suggest that the effective proton charge for high-multipole, and , transitions is quenched to approximately two-thirds of the collective value. Correlations between nucleons may offer an explanation of this unexpected phenomenon, which is in stark contrast to the collective nature of lower-multipole, electric transitions observed in atomic nuclei.