posted on 2018-05-15, 15:39authored byZ. Podolyák, C. M. Shand, N. Lalović, J. Gerl, D. Rudolph, T. Alexander, P. Boutachkov, M. L. Cortés, M. Górska, I. Kojouharov, N. Kurz, C. Louchart, E. Merchán, C. Michelagnoli, R. M. Pérez-Vidal, S. Pietri, D. Ralet, M. Reese, H. Schaffner, C. Stahl, H. Weick, F. Ameil, G. de Angelis, T. Arici, R. Carroll, Z. Dombrádi, A. Gadea, P. Golubev, M. Lettmann, C. Lizarazo, D. Mahboub, H. Pai, Z. Patel, N. Pietralla, P. H. Regan, L. G. Sarmiento, O. Wieland, Emma Wilson, B. Birkenbach, B. Bruyneel, I. Burrows, L. Charles, E. Clément, F. C. L. Crespi, D. M. Cullen, P. Désesquelles, J. Eberth, V. González, T. Habermann, L. Harkness-Brennan, H. Hess, D. S. Judson, A. Jungclaus, W. Korten, M. Labiche, A. Maj, D. Mengoni, D. R. Napoli, A. Pullia, B. Quintana, G. Rainovski, P. Reiter, M. D. Salsac, E. Sanchis, J. J. Valiente Dóbon
The ^{54}Fe nucleus was populated from a ^{56}Fe beam impinging on a Be target with an energy of E/A=500 MeV. The internal decay via γ-ray emission of the 10^{+} metastable state was observed. As the structure of this isomeric state has to involve at least four unpaired nucleons, it cannot be populated in a simple two-neutron removal reaction from the ^{56}Fe ground state. The isomeric state was produced in the low-momentum (-energy) tail of the parallel momentum (energy) distribution of ^{54}Fe, suggesting that it was populated via the decay of the Δ^{0} resonance into a proton. This process allows the population of four-nucleon states, such as the observed isomer. Therefore, it is concluded that the observation of this 10^{+} metastable state in ^{54}Fe is a consequence of the quark structure of the nucleons.
History
Citation
Physical Review Letters, 2016, 117, 222302
Author affiliation
/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/Department of Mathematics