The “island of inversion" from a nuclear moments perspective and the g factor of 35Si

The European Physical Journal Special Topics - Tập 150 - Trang 149-153 - 2007
G. Neyens1, P. Himpe1, D. L. Balabanski2, P. Morel3, L. Perrot4, M. De Rydt1, I. Stefan4, C. Stodel4, J. C. Thomas4, N. Vermeulen, D. T. Yordanov1
1Katholieke Universiteit Leuven, Leuven, Belgium
2Institute for Nuclear Research and Nuclear Energy, Bulgarian Academy of Sciences, Sofia, Bulgaria
3CEA/DIF/DPTA/PN, Bruyères-le-Châtel, France
4GANIL, BP. 55027, Caen Cedex 5, France

Tóm tắt

This paper reviews recent results from electromagnetic moment measurements on isotopes in the island of inversion around N=20. The obtained moments on neutron rich Na, Mg, Al and Si isotopes allow to draw conclusions on the amount of intruder components in their ground state wave function, demonstrating a gradual transition from the normal sd-shell region into the island of inversion, starting at N=18 for Na, N=19 for Mg and N=20 for Al isotopes. A measurement of the ground state g factor of 35Si (N=21), using a polarized fragment beam at GANIL, is discussed in more detail. The magnetic moment μ(35Si, Iπ= 7/2-) = (-)1.638(4) μN is consistent with a normal ground state structure, dominated by a νf7/2 neutron.

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