Precision mass measurements of magnesium isotopes and implications on the validity of the Isobaric Mass Multiplet Equation
arXiv:1707.07714 · doi:10.1103/PhysRevC.96.034316
Abstract
If the mass excess of neutron-deficient nuclei and their neutron-rich mirror partners are both known, it can be shown that deviations of the Isobaric Mass Multiplet Equation (IMME) in the form of a cubic term can be probed. Such a cubic term was probed by using the atomic mass of neutron-rich magnesium isotopes measured using the TITAN Penning trap and the recently measured proton-separation energies of Cl and Ar. The atomic mass of Mg was found to be within 1.6 of the value stated in the Atomic Mass Evaluation. The atomic masses of Mg were measured to be both within 1, while being 8 and 34 times more precise, respectively. Using the Mg mass excess and previous measurements of Cl we uncovered a cubic coefficient of = 28(7) keV, which is the largest known cubic coefficient of the IMME. This departure, however, could also be caused by experimental data with unknown systematic errors. Hence there is a need to confirm the mass excess of S and the one-neutron separation energy of Cl, which have both come from a single measurement. Finally, our results were compared to ab initio calculations from the valence-space in-medium similarity renormalization group, resulting in a good agreement.
7 pages, 3 figures
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