Isobaric multiplet mass equation in the $A=31$ $T = 3/2$ quartets (1607.00690v1)
Abstract: The observed mass excesses of analog nuclear states with the same mass number $A$ and isospin $T$ can be used to test the isobaric multiplet mass equation (IMME), which has, in most cases, been validated to a high degree of precision. A recent measurement [Kankainen et al., Phys. Rev. C 93 041304(R) (2016)] of the ground-state mass of ${31}$Cl led to a substantial breakdown of the IMME for the lowest $A = 31, T = 3/2$ quartet. The second-lowest $A = 31, T = 3/2$ quartet is not complete, due to uncertainties associated with the identity of the ${31}$S member state. Using a fast ${31}$Cl beam implanted into a plastic scintillator and a high-purity Ge $\gamma$-ray detection array, $\gamma$ rays from the ${31}$Cl$(\beta\gamma)$${31}$S sequence were measured. Shell-model calculations using USDB and the recently-developed USDE interactions were performed for comparison. Isospin mixing between the ${31}$S isobaric analog state (IAS) at 6279.0(6) keV and a nearby state at 6390.2(7) keV was observed. The second $T = 3/2$ state in ${31}$S was observed at $E_x = 7050.0(8)$ keV. Isospin mixing in ${31}$S does not by itself explain the IMME breakdown in the lowest quartet, but it likely points to similar isospin mixing in the mirror nucleus ${31}$P, which would result in a perturbation of the ${31}$P IAS energy. USDB and USDE calculations both predict candidate ${31}$P states responsible for the mixing in the energy region slightly above $E_x = 6400$ keV. The second quartet has been completed thanks to the identification of the second ${31}$S $T = 3/2$ state, and the IMME is validated in this quartet.
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