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The 'island of inversion' from a nuclear moments perspective and the g factor of Si-35

机译:从核矩角度看“反转岛”和Si-35的g因子

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摘要

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 Si-35 (N=21), using a polarized fragment beam at GANIL, is discussed in more detail. The magnetic moment mu(Si-35, I-pi = 7/2(-)) = (-)1.638(4) mu(N) is consistent with a normal ground state structure, dominated by a nu f(7/2) neutron.
机译:本文回顾了N = 20附近反演岛中同位素的电磁矩测量的最新结果。在富含中子的Na,Mg,Al和Si同位素上获得的力矩可以得出入侵者在其基态波函数中的数量的结论,表明从正常的sd壳区域到反演岛逐渐过渡,始于对于Na,N = 18,对于Mg,N = 19,对于Al同位素,N = 20。使用GANIL上的极化碎片光束对Si-35(N = 21)基态g因子的测量进行了更详细的讨论。磁矩mu(Si-35,I-pi = 7/2(-))=(-)1.638(4)mu(N)与以nu f(7/2)为主的正常基态结构一致)中子。

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