Isobaric multiplet mass equation in the A=31 T=3/2 quartets

Isobaric multiplet mass equation in the $A=31$ $T = 3/2$ quartets

Abstract

Background: The observed mass excesses of analog nuclear states with the same mass number and isospin 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 Cl led to a substantial breakdown of the IMME for the lowest quartet. The second-lowest quartet is not complete, due to uncertainties associated with the identity of the S member state.

Purpose: Our goal is to populate the two lowest states in S and use the data to investigate the influence of isospin mixing on tests of the IMME in the two lowest quartets.

Methods: Using a fast Cl beam implanted into a plastic scintillator and a high-purity Ge -ray detection array, rays from the ClS sequence were measured. Shell-model calculations using USDB and the recently-developed USDE interactions were performed for comparison.

Results: Isospin mixing between the S isobaric analog state (IAS) at 6279.0(6) keV and a nearby state at 6390.2(7) keV was observed. The second state in S was observed at keV. Calculations using both USDB and USDE predict a triplet of isospin-mixed states, including the lowest state in P, mirroring the observed mixing in S, and two isospin-mixed triplets including the second-lowest states in both S and P.

Conclusions: Isospin mixing in 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 P, which would result in a perturbation of the P IAS energy. USDB and USDE calculations both predict candidate P states responsible for the mixing in the energy region slightly above keV. The second quartet has been completed thanks to the identification of the second S state, and the IMME is validated in this quartet.


PACS numbers: 21.10.Hw, 21.60.Cs, 23.20.Lv, 27.30.+t

I Introduction

Due to the charge-independent nature of the strong nuclear force, it is possible to model the proton and neutron as spin-like “isospin” states of a single particle, the nucleon. This isospin model treats both the proton and the neutron as degenerate particles with isospin , but with opposite isospin projections: for neutrons and for protons Heisenberg (1932). Thus, nuclei that share a given total mass number can be seen as total projection states, each with , where and are the number of neutrons and protons, respectively. Each energy level in a given nucleus itself possesses a total isospin , so it is possible to treat analogous states in isobaric nuclei as members of a -member multiplet, each with the same and a different isospin projection .

Under this symmetric formalism, analogous energy states with the same isospin have exactly the same mass excess values . However, electrostatic effects perturb the energies of nuclear analog states with differing numbers of protons, breaking this degeneracy and resulting in systematically different energies for multiplet members. First proposed by Wigner, the isobaric multiplet mass equation (IMME) Wigner (1957); Weinberg and Treiman (1959) is a model that uses first-order perturbation theory to predict that the mass excesses of nuclear isobaric analog states (IAS) within an isospin multiplet are systematically related by their isospin projections according to the following quadratic equation:

(1)

where , , and are coefficients that can either be calculated using the perturbation theory or obtained from a quadratic fit of the measured mass excesses of the multiplet members. The IMME can thus be used to predict the energies of unobserved multiplet states, and measurements of these states can be compared with the quadratic form of the IMME in order to test its validity. A breakdown of the IMME could indicate a failure of the perturbation theory and a need for higher-order terms, the presence of many-body charge-dependent forces Jänecke (1969), isospin mixing of the IAS with other nearby states of different isospin Signoracci and Brown (2011), or inaccurate measurements.

Historically, the IMME has been very successful at describing experimental values, requiring very few deviations from the quadratic form. As discussed in Refs. Britz et al. (1998) and Lam et al. (2013), in situations where the fit of the quadratic form is very poor, a cubic or quartic form with extra terms or may be required. Typically, these terms have been determined empirically to be either very small, 1 keV, or consistent with zero. A number of situations where a term has been required are noted in Ref. MacCormick and Audi (2014), including the and quintets and the and quartets; these and other cases are discussed here.

In the quintet mentioned above, multiple studies Britz et al. (1998); Charity et al. (2011) have noted the need for a significant cubic term in the IMME, and keV for Refs. Britz et al. (1998) and Charity et al. (2011), respectively. The recent evaluation of Ref. MacCormick and Audi (2014) confirmed that a quartic function was most likely an even better fit to the data and suggested the need for both theoretical and experimental studies of the multiplet members to address the IMME breakdown. A Penning trap measurement of multiple isotopes including Mg Gallant et al. (2014) reported breakdowns of the IMME for the and quartets, requiring cubic terms of keV and keV, respectively. The quintet is currently the most precisely measured quintent. Here, a precise Penning trap measurement of Si Kwiatkowski et al. (2009) led to an observed breakdown of the IMME, requiring a small, but very significant, cubic term keV, which was supported by a measurement of the Cl mass using the S(He,)Cl reaction Wrede et al. (2010). A later precision measurement of the S mass Kankainen et al. (2010) led to an even greater precision on the Cl mass excess and found that no combination of various literature values could produce a fit that validated the IMME for the quintet. A recent review of mass measurements Kankainen et al. (2012) suggested that new mass measurements of other multiplet members might revalidate the IMME in this quintet, and a theoretical study of the quintet Signoracci and Brown (2011) demonstrated that the IMME deviation, as well as the observed isospin-forbidden proton decay from the Cl IAS and a correction to the superallowed decay from Ar, could be traced to isospin mixing of the states with states. In the case, a relatively large coefficient of keV was clearly required to fit the data. Although no definite solution has been found yet, both inaccurate experimental data and isospin mixing have been suggested as potential causes for the breakdown Yazidjian et al. (2007).

In several instances of IMME breakdown, additional study has revalidated the quadratic IMME. Reference Gallant et al. (2014) reported, in addition to the findings on Mg, a new Mg mass and a resulting IMME breakdown requiring a cubic term of 2.8(11) keV for the quintent. In this case, a recent experimental measurement of Mg decay Glassman et al. (2015) used the superallowed transition to the Na IAS and the state’s subsequent decay to deduce an excitation energy for the IAS. This result was 28 times more precise than the previous measurement and, together with the ground state mass excess of Na, was shown to revalidate the IMME for the quintet. A storage ring mass measurement of a number of shell nuclei, including Ni Zhang et al. (2012), found that an IMME fit of the lowest quartet required an enormous cubic term of keV, a deviation from the quadratic IMME. In this latter case, as in the case, the IMME was revalidated after a measurement of Ni -delayed decay Su et al. (2016) which produced a more precise Co IAS excitation energy and a cubic IMME fit with a coefficient compatible with zero. In the case mentioned above, a relatively large coefficient of keV was required to fit the IMME. This anomaly was found through high-precision mass measurements of Li and Be to be the result of isospin mixing in B and Be Brodeur et al. (2012).

In the lowest , quartet, it has until recently been difficult to test the IMME because the experimental mass excess value of Cl has been relatively imprecise. A 1977 experimental measurement of the Ar(He,Li)Cl value resulted in a mass excess value of keV Benenson et al. (1977). Subsequent evalutions of the IMME Benenson and Kashy (1979); Britz et al. (1998); Lam et al. (2013); MacCormick and Audi (2014) have included adjusted central values of this mass excess, but the uncertainty has remained. In contrast to high-precision mass excess and excitation energy values of the relevant states in S Moalem and Wildenthal (1973); Kankainen et al. (2010, 2006) and P Redshaw et al. (2008); Ouellet and Singh (2013) (based on mass measurements of those nuclei and experimental measurements of their excitation energies) and in Si (based on mass measurements of Si Rainville et al. (2005) and neutron-capture reaction measurements linking the isotopes from Si to Si Islam et al. (1990); Raman et al. (1992); Röttger et al. (1997)), the 50-keV uncertainty in the Cl mass excess has hindered attempts to test the IMME stringently in the lowest quartet. A recent Penning trap mass measurement of Cl finally obtained a value for the ground state mass excess 15 times more precise than previous estimates Kankainen et al. (2016), leading to an IMME breakdown in the lowest quartet; the IMME fit required an unusually large cubic term, with keV.

Similar to the lowest quartet, uncertainties associated with both the energy of the first excited state in Cl and the identity of the second state in S have precluded a quality test of the IMME in the second quartet. In fact, a tentative measurement of the first Cl excited state via Ar decay Axelsson et al. (1998) was the only evidence for the observation of that state Wrede et al. (2009a) until a recent Coulomb-breakup experiment was performed to confirm the existence of the state Langer et al. (2014). The excitation energy was found in Ref. Langer et al. (2014) to be keV, leaving the identity of the second state in S as the primary ambiguity in the quartet. Various sources have reported excitation energies for the S state ranging from a definite assignment for a state at keV using the Si(He,)S reaction Davidson et al. (1975) with somewhat low precision to a relatively precise, but tentative, assignment for a state at keV Wrede et al. (2009b), with alternative candidates at 6975(3) Brown et al. (2014); Wrede et al. (2009b) and 7053(2) keV Wrede et al. (2009b).

Although this S state is expected to be nearly 1 MeV above the proton threshold, the proton emission is isospin forbidden and, therefore, it should have a substantial -decay branch unlike the other low-spin levels in the region Glassman et al. (2015). Precise observation of a high energy -ray transition from a low-spin state in this region would be a signature of the second state, allowing for a precise determination of its energy. The shell model predicts that the state decays predominantly to the ground state, and shell model calculations using the universal -shell version “B” (USDB) Richter et al. (2008) and the recently-developed version “E” (USDE) Bennett et al. (2016) models predict a S state 745(50) keV above the S IAS energy of keV. In the shell model, this state has a Cl feeding of 0.03(2)% and a ground-state -decay branch of .

The present paper reports the results from a Cl -decay study and presents potential solutions to the problem of IMME breakdown for the lowest quartet based on the observation of isospin mixing in S. In addition, a precision measurement of the second S state is reported, allowing for the most stringent test of the IMME to date for the second quartet.

Ii Experiment

The present experiment is one in a series of recent -delayed -decay experiments to investigate the shell using fast neutron-deficient beams at the National Superconducting Cyclotron Laboratory Bennett et al. (2013); Schwartz et al. (2015); Pérez-Loureiro et al. (); Bennett et al. (2016); Glassman et al. (2015). In particular, the -delayed decay of Cl was measured using an experimental procedure that was already described in Bennett et al. (2016). Briefly, a fast beam of up to 9000 Cl ions per second was implanted into a plastic scintillator, which acted as a -decay trigger. The -delayed rays were detected using the Clovershare array: nine “clover” detectors of four Ge crystals each, surrounding the plastic scintillator. Data from the crystals were gain-matched and calibrated to produce and spectra, the latter of which were gated on a variety of deexciting rays. From these data, a decay scheme was constructed including the observed S levels and their excitation energies and feedings. Absolute intensities for the observed rays were also determined. In the present work we focus on the states.

Iii Results and Discussion

iii.1 First Quartet

Experimental Results

We observed the -ray deexcitation of a S state at keV, as previously reported in Ref. Bennett et al. (2016). Neither the feeding nor the -decay branching of the state match our USDB predictions Richter et al. (2008) without isospin mixing, and the state’s feeding was abnormally high for a state at such a high energy. By computing the Fermi strengths for both the S IAS at 6279.0(6) keV and this state, it was discovered that the two states were mixing isospin strongly. The mixing of the state at 6390 keV allowed for an unambiguous spin and parity identification of . The positive identification of the state has implications for the P()S reaction rate in the astrophysical environment of a classical nova outburst; these findings are discussed in Ref. Bennett et al. (2016). Excitation energies, -decay energies, and feedings of the two states are summarized in Table 1.

Imme

Here we explore the impact of isospin mixing on the IMME for the lowest quartet. In order to use the IMME fit, we needed values for both the ground-state mass excesses of the multiplet members and the S and P IAS excitation energies. For the lowest quartet, we used the values in Ref. Kankainen et al. (2016) for Cl, P, and Si. For S, we used the value for the S IAS excitation energy obtained from the present work Bennett et al. (2016) rather than the value of keV used in Ref. Kankainen et al. (2016), which is from the Nuclear Data Sheets (NDS) Ouellet and Singh (2013). The value in Ref. Ouellet and Singh (2013) is based on a fit of gamma-ray energies from a measurement of Cl beta decay Saastamoinen (2011). However, since the NDS value does not factor in the 1.5-keV systematic uncertainty reported in Ref. Saastamoinen (2011), we considered it to be less precise than the value obtained in the present work Bennett et al. (2016), which includes both statistical and systematic uncertainty. Nevertheless, it is worthwhile to note that the excitation energy value from the present work is consistent with the value from Refs. Ouellet and Singh (2013); Saastamoinen (2011) when systematic uncertainties are included.

As discussed in Ref. Kankainen et al. (2016), with the new high-precision Cl mass excess, a fit of the quadratic IMME fails, requiring a large coefficient for the cubic term, keV. Using our value of 6279.0(6) keV for the observed IAS excitation energy, the quadratic fit also fails, requiring a coefficient for the cubic term of keV. This failure of the quadratic fit is independent of whether we use our value for the S excitation energy or the value from Ref. Saastamoinen (2011). The inputs and outputs of this fit are reported in Tables 2 and 3, respectively.

The authors of Ref. Kankainen et al. (2016) hypothesize that isospin mixing could help explain the observed IMME breakdown. In the case where two states mix, the following equations may be used to calculate the empirical mixing matrix element and unperturbed level spacing:

(2)
(3)
(4)
(5)
(6)

where is the observed spacing, is the unperturbed level spacing, is the mixing matrix element, is the perturbation, and may be calculated from the Fermi strengths of -decay transitions to the two mixed states (Eq. 4). With these equations and the Fermi strengths calculated in Ref. Bennett et al. (2016) [ and ], we derive an empirical mixing matrix element and unperturbed level spacing of 41(1) and 74(2) keV, respectively. Using this unperturbed level spacing and the observed energies of the two states, we calculate the unperturbed energy of the IAS to be 6297.6(13) keV.

In order to test the hypothesis that isospin mixing is affecting the quadratic IMME fit in the lowest quartet, we tried fitting the IMME including this unperturbed S IAS energy along with the new Cl mass measured in Ref. Kankainen et al. (2016) and the other, precisely known values for Si and P Wang et al. (2012). However, this does little to fix the breakdown problem: the reduced chi-squared value of the quadratic fit actually increases from , in Ref. Kankainen et al. (2016), and 16.0, using the new observed IAS , to 17.0. For the cubic fit, the coefficient also becomes larger in magnitude, changing from keV or keV to keV. Input energies for the unperturbed-energy fits from the present work are listed in Table 4, and fit output parameters for the quadratic and cubic fit are listed in Table 5. Residuals for the quadratic fit are shown in Fig. 1.

(keV) (keV) (%)
Table 1: Experimentally determined excitation energies , -decay energies , and Cl -decay feedings for the first two S states, as well as the 6390-keV state that mixes with the first state.
Nucleus (keV) (keV)
Cl
S
P
Si
Table 2: Ground-state mass excess and excitation energy values used as input for the IMME fits of the lowest quartet. Except for the observed excitation energy of the S IAS, which is from Ref. Bennett et al. (2016), all values are the same as in Ref. Kankainen et al. (2016).
Quadratic Cubic
Table 3: Output coefficients for the quadratic and cubic IMME fits for the lowest quartet using input data from Table 2. All coefficient values are in units of keV. The cubic fit did not contain any degrees of freedom, so the value is undefined and hence ommitted.
Nucleus (keV) (keV)
Cl
S
P
Si
Table 4: Ground-state mass excess and excitation energy values used as input for the IMME fits of the lowest quartet. Except for the unperturbed excitation energy of the S IAS, which is from the present work Bennett et al. (2016), all values are the same as in Kankainen et al. (2016).
Quadratic Cubic
Table 5: Output coefficients for the quadratic and cubic IMME fits for the lowest quartet using input data from Table 4. All coefficient values are in units of keV.
Figure 1: Residuals for the quadratic IMME fit of the lowest quartet (Tables 4 and 5) after accounting for the observed isospin mixing in S.

Given the observed isospin mixing in S, it is likely that there is similar mixing present in the mirror nucleus P, which has not yet been directly observed. Using the unperturbed energy of the S IAS from Ref. Bennett et al. (2016) and the results of Ref. Kankainen et al. (2016), the IMME can be used to predict an “unperturbed” energy for the lowest state in P of 6390.8(24) keV, only keV higher than the current energy value of the P IAS, keV. If this state, like the S IAS, mixes isospin with a nearby higher-energy state, its unperturbed energy could be high enough to revalidate the IMME for the quartet after accounting for the isospin mixing.

At first glance, however, it appears that no such state is known to exist experimentally. No nearby higher-energy states listed in the 2013 Nuclear Data Sheets Ouellet and Singh (2013) have the same spin and parity () as the P IAS. It is possible, however, to derive combinations of excitation energy and mixing matrix element for such a state that would revalidate the quadratic IMME. Using Eqs. 2 and 5 along with the observed and predicted energies of the lowest P state and solving for , the result is a curve for keV (Fig. 2). The lowest energy solution at 6401 keV corresponds to two degenerate unperturbed states at keV, perturbed by 10 keV by mixing.

As a naive empirical prediction, the assumption that the unperturbed energy spacing is identical in this case to the S case ( keV) yields a second state at keV, with an associated mixing matrix element of 27.2(35) keV. Coincidentally, this predicted energy is near a known P state at 6460.8(16) keV, listed as in Ref. Ouellet and Singh (2013). Although some sources Endt (1990) have committed to a definite spin and parity assignment for this state, multiple experimental studies Wolff and Leighton (1970); Al-Jadir et al. (1980); McCulloch et al. (1984); Vernotte et al. (1990, 1999), while potentially favoring the assignment, have not excluded a assignment. Further, as noted in Ref. Ouellet and Singh (2013), another study Kaschl et al. (1969) has even labeled the state as , further complicating the matter of its spin and parity. If the state did in fact have , it could mix with the IAS at 6381 keV.

Figure 2: Isospin mixing matrix element, including confidence band, of a hypothetical state engaged in isospin mixing with the P IAS at 6381 keV as a function of the observed excitation energy of the second state. The band is derived under the assumption that the IMME provides a good fit of the data after accounting for isospin mixing. The dotted (left) and dot-dashed (right) lines show the 1 bounds obtained using this prediction when the USD mixing matrix element and 6461-keV state energy, respectively, are used as inputs.

Shell Model

In order to facilitate the search for the hypothetical state mixing with the P IAS, we have used both USDE and USDB to predict energy levels and mixing matrix elements for the P IAS and its nearby states. As in the S case, both USDE and USDB predict a triplet of states involved in mixing. The results of both the USDE and USDB calculation are reported in Table 6. The mixing matrix element values obtained are substantially smaller than those for S Bennett et al. (2016). While there are experimental candidates for the lower state in the triplet at 6233 keV and 6158 keV Ouellet and Singh (2013), again no higher state in the vicinity is immediately apparent. The closest candidate is the state previously mentioned at 6461 keV, but as it requires a relatively high mixing matrix element (27(3) keV) compared to theory (Fig. 2), it should be regarded as a tentative solution at best. Consequently, experimental searches for additional levels are needed to test the likelihood that the 6461-keV state is the state mixing with the P IAS and to find other potential states which could fulfill that role. The shell-model matrix elements for the mixed states (Table 6) and the functional form in Fig. 2 may be used to predict the energy region in which the mixed state is likely to exist: the theoretical upper and lower bounds are and 6406 keV, respectively. Searches for the hypothetical mixing state should thus focus on the region slightly above keV.

USDB USDB USDE USDE
Table 6: Calculated excitation energies and mixing matrix elements of the triplet of isospin-mixed states including the lowest state in P for both USDB and USDE interactions. The matrix elements listed are between the listed state and the state. All values are in units of keV.
Figure 3: High-energy portion of the Cl -coincident spectrum obtained in Ref. Bennett et al. (2016). The transitions from the IAS at 6279 keV, the state at 6390 keV, and the S state at 7050 keV to the ground state are all labeled with a vertical line. The peak marked with an asterisk at 6539 keV is the first escape peak corresponding to the 7050-keV transition. The peak at 6791 keV is the sum peak between the strong 6280-keV photopeak Bennett et al. (2016) and the 511 keV annihilation photopeak. The peak at 6255 keV is a photopeak corresponding to a transition from a S state to the ground state.
Figure 4: Residuals for the quadratic IMME fit of the second-lowest quartet (Tables 7 and 8).
Nucleus (keV) (keV)
Cl
S
P
Si
Table 7: Ground-state mass excess and excitation energy values Ouellet and Singh (2013) used as input for the IMME fits of the second-lowest quartet.
Quadratic Cubic
Table 8: Output coefficients for the quadratic and cubic IMME fits for the second-lowest quartet using input data from Table 7. All coefficient values are in units of keV.

iii.2 Second Quartet

Experimental Results

An isolated -ray peak corresponding to a laboratory energy was observed in our spectrum (Fig. 3), 770 keV above the IAS, as predicted for the second S state by our shell model calculations. It did not appear in any of our coincidence spectra, so the simplest interpretation is that this transition is from a S level at keV undergoing a transition to the ground state. The feeding of 0.047(5)% for this state is consistent with shell model predictions, and no other -ray transitions de-exciting this state were observed, implying that it decays predominantly to the ground state. The agreement of the state’s excitation energy and feeding with the shell-model prediction, its singular branch to the ground state, and a small observed - branch Wrede et al. (2009a) all provide evidence that it is indeed the second state, with , in S.

Imme

A quadratic fit of the IMME using the observed 7050-keV state energy and the energies of the other three quartet members results in a good fit with and a value of 0.48. This is further confirmation that the S state at 7050 keV is the S member of the second quartet. Input mass excesses and excitation energies are reported in Table 7. Output parameters for both the quadratic and cubic fits are reported in Table 8. Residuals for the quadratic fit of all four states are shown in Fig. 4.

S USDB USDB USDE USDE
P USDB USDB USDE USDE
Table 9: Calculated excitation energies and mixing matrix elements of the triplets of states involved in mixing with the second-lowest states in both S and P, for both USDB and USDE interactions. The matrix elements listed are between the listed state and the state. All values are in units of keV.

Although the IMME fit is very good with the measured mass excesses and excitation energies for the second quartet members, it is possible that a small amount of undetected isospin mixing occurs, similar to the mixing in the lowest quartet. While potential candidate states exist for mixing in each of these nuclei, no experimental evidence was observed to positively identify such a state in S. For example, no -ray transitions were observed for any states between keV and keV in either the or the coincidence spectra.

Shell Model

To estimate the amount of mixing that might occur, we have used both the USDE and USDB calculations to predict energy levels and mixing matrix elements for both S and P (Table 9). Both models produce small mixing matrix elements, consistent with the implication from our IMME fit that the mixing is small, with the lack of observation of other -ray branches in the energy region, and with the small ratio of proton emission to decay of the 7050-keV state.

Prediction of Cl First Excited State Energy

Using our high-precision measurement of the excitation energy of the second state in S, it is possible to predict the energy of the first excited Cl state with a higher precision. Using the S, P, and Si input mass excess values and excitation energies in Table 4 to produce the IMME curve, and accounting for the uncertainty introduced by the possibility of isospin mixing via the coefficient in the cubic fit, the resulting IMME mass excess is keV. When combined with the known Cl ground state mass excess from Ref. Kankainen et al. (2016) and its uncertainty, the predicted excitation energy of the state is keV, consistent with the measured value of keV Langer et al. (2014). It is also possible to calculate the energy of the state using the S resonance energy based on the measurement, Wrede et al. (2009a); Axelsson et al. (1998) and the recent value of the proton separation energy, Kankainen et al. (2016): The result is , which is consistent with our prediction within 1.8 combined standard deviations and with the value from Ref. Langer et al. (2014) within 1.6 combined standard deviations. Given the slight tension between the value based on the measurement Axelsson et al. (1998) and the other two values, a new measurement of Ar decay Koldste et al. (2013, 2014) with high sensitivity to low-energy protons would be an interesting study.

Iv Conclusions

The problem of IMME breakdown in the lowest quartet may be a result of isospin mixing in one or more of the multiplet members. We have measured the excitation energy of the S IAS and found that it is isospin mixed with a nearby state. However, we have shown that the isospin mixing in S alone cannot explain the IMME breakdown observed in Ref. Kankainen et al. (2016), but that incorporating similar mixing in P could account for the breakdown. Better experimental data are needed to search for the hypothesized P state that may be mixing with the IAS. The state at 6461 keV is the best existing candidate for this state, but is not consistent with shell model predictions and should be investigated further. It is not certain that every P state in the energy region has been observed. Future experiments could focus on gamma spectroscopy of this region in P to complement the numerous charged particle reaction measurements carried out to-date. The question of isospin mixing in P likely holds the key to explaining the IMME breakdown in the lowest quartet; uncovering the structure in the important energy region slightly above keV could lead to a deeper understanding of the perturbative effects of isospin mixing on this widely-used theoretical model.

In addition, the clear identification of the second S state at 7050 keV in the present work has completed the second quartet. Three of the four quartet member states now have mass-excess uncertainties keV and their masses are well-described by the quadratic form of the IMME. Further studies of this multiplet could focus on reducing the uncertainty of the energy of the first excited Cl state. A new Ar decay study could provide an independent measurement of the -delayed proton energy, and in-beam ray spectroscopy, while challenging due to the very small expected -decay branching ratio of the state, might present a novel approach to measuring the excitation energy of this state.

The researchers gratefully acknowledge the dedicated effort of the NSCL operations staff to ensure the delivery of multiple very pure beams. This work was supported by the U.S. National Science Foundation under Grants No. PHY-1102511, PHY-1404442, PHY-1419765, and PHY-1431052, the US Department of Energy, National Nuclear Security Administration under Grant No. DE-NA0000979, and the Natural Sciences and Engineering Research Council of Canada. We also gratefully acknowledge use of the Yale Clovershare array.

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