Charge radii of exotic potassium isotopes challenge nuclear theory and the magic character of N = 32

Nuclear charge radii are sensitive probes of different aspects of the nucleon–nucleon interaction and the bulk properties of nuclear matter, providing a stringent test and challenge for nuclear theory. Experimental evidence suggested a new magic neutron number at N = 32 (refs. 1–3) in the calcium region, whereas the unexpectedly large increases in the charge radii4,5 open new questions about the evolution of nuclear size in neutron-rich systems. By combining the collinear resonance ionization spectroscopy method with β-decay detection, we were able to extend charge radii measurements of potassium isotopes beyond N = 32. Here we provide a charge radius measurement of 52K. It does not show a signature of magic behaviour at N = 32 in potassium. The results are interpreted with two state-of-the-art nuclear theories. The coupled cluster theory reproduces the odd–even variations in charge radii but not the notable increase beyond N = 28. This rise is well captured by Fayans nuclear density functional theory, which, however, overestimates the odd–even staggering effect in charge radii. These findings highlight our limited understanding of the nuclear size of neutron-rich systems, and expose problems that are present in some of the best current models of nuclear theory. The charge radii of potassium isotopes up to 52K are measured, and show no sign of magicity at 32 neutrons as previously suggested in calcium. The observations are interpreted with coupled cluster and density functional theory calculations.

Nuclear charge radii are sensitive probes of different aspects of the nucleon-nucleon interaction and the bulk properties of nuclear matter; thus, they provide a stringent test and challenge for nuclear theory.The calcium region has been of particular interest, as experimental evidence has suggested a new 'magic' number at N = 32 [1][2][3], while the unexpectedly large increases in the charge radii [4,5] open new questions about the evolution of nuclear size in neutron-rich systems.By combining the collinear resonance ionization spectroscopy method with β-decay detection, we were able to extend the charge radii measurement of potassium (Z = 19) isotopes up to the exotic 52 K (t 1/2 = 110 ms), produced in minute quantities.
Our work provides the first charge radii measurement beyond N = 32 in the region, revealing no signature of the magic character at this neutron number.The results are interpreted with two state-of-the-art nuclear theories.For the first time, a long sequence of isotopes could be calculated with coupled-cluster calculations based on newly developed nuclear interactions.The strong increase in the charge radii beyond N = 28 is not well captured by these calculations, but is well reproduced by Fayans nuclear density functional theory, which, however, overestimates the odd-even staggering effect.These findings highlight our limited understanding on the nuclear size of neutron-rich systems, and expose pressing problems that are present in some of the best current models of nuclear theory.
The charge radius is a fundamental property of the atomic nucleus.Though it globally scales with the nuclear mass as A 1/3 , the nuclear charge radius additionally exhibits appreciable isotopic variations that are the result of complex interactions between protons and neutrons.Indeed, charge radii reflect various nuclear structure phenomena such as halo structures [6,7], shape staggering [8] and shape coexistence [9], pairing correlations [10,11], neutron skins [12] and the occurrence of nuclear magic numbers [5,13,14].The term 'magic number' refers to the number of protons or neutrons corresponding to completely filled shells, thus resulting in an enhanced stability and a relatively small charge radius.
In the nuclear mass region near potassium, the isotopes with neutron number N = 32 are proposed to be 'magic', based on an observed sudden decrease in binding energy beyond N = 32 [2,3] and high excitation energy of the first excited state in 52 Ca [1].The nuclear charge radius is also a sensitive indicator of 'magicity': a sudden increase in the charge radii of isotopes is observed after crossing the classical neutron magic numbers N = 28, 50, 82 and 126 [5,[13][14][15].Therefore, the experimentally observed strong increase in the charge radii between N = 28 and N = 32 of calcium [4] and potassium chains [5], and in particular the large radius of 51 K and 52 Ca (both having 32 neutrons) have attracted significant attention.
One aim of the present study is therefore to shed light on several open questions in this region: how does the nuclear size of very neutron-rich nuclei evolve, and is there any evidence for the 'magicity' of N = 32 from nuclear size measurement?We furthermore provide new data to test several newly developed nuclear models, which aim at understanding the evolution of nuclear charge radii of exotic isotopes with large neutron-toproton imbalance.So far, all ab initio nuclear methods, allowing for systematically improvable calculations based on realistic Hamiltonians with nucleon-nucleon and three-nucleon potentials, have failed to explain the enhanced nuclear sizes beyond N = 28 in the calcium isotopes [4,16].Meanwhile, nuclear Density Functional Theory (DFT) using Fayans functionals has been successful in predicting the increase in the charge radii of isotopes in the proton-magic calcium chain [11], as well as the kinks in the proton-magic tin and lead [13].These state-of-the-art theoretical approaches have been predominantly used to study the charge radii of even-Z isotopes, and only very recently could charge radii of odd-Z Cu (Z = 29) isotopes be investigated with Abody in-medium similarity renormalization group (IM-SRG) method and Fayans-DFT [10].
Laser spectroscopy techniques yield the most accurate and precise measurements of the charge radius for radioactive nuclei.These highly efficient and sensitive experiments at radioactive ion beam facilities have expanded our knowledge of nuclear charge radii distributed throughout the nuclear landscape [17].Laser spectroscopy achieves this in a nuclear-modelindependent way by measuring the small perturbations of the atomic hyperfine energy levels due to the electromagnetic properties of the nucleus.Although these hyperfine structure (hfs) effects are as small as one part in a million compared to the total transition frequency, they can nowadays be measured with remarkable precision and efficiency, even for shortlived, weakly-produced, exotic isotopes [10].
To enhance the sensitivity of the high-resolution, optically detected collinear laser spectroscopy method that was previously used to measure the mean-square charge radii of the potassium isotopes [5,18,19], we used the Collinear Resonance Ionization Spectroscopy (CRIS) experimental setup at the ISOLDE facility of CERN.This allows very exotic isotopes to be studied with the same resolution as the optically detected method [10,20].Relevant details of the ISOLDE radioactive beam facility and the CRIS setup are depicted in Fig. 1 (see Methods for details).The CRIS method relies on the step-wise resonant laser excitation and ionization of atoms.For this experiment, a narrowband laser was used to excite potassium atoms from one of the hfs components of the atomic ground state into a hyperfine energy level of an excited state.From there, another excitation and subsequent laser ionization were induced by broadband high-power laser beams, as discussed in Ref. [21].The resulting ions were deflected from the remaining (neutral) particles in the beam, and were detected with an ion detector.This method allows nearly background-free ion detection, and thus has very high sensitivity, provided that the contaminating beam particles are not ionized (through e.g.collisional ionisation or due to the highpower non-resonant laser beams).By counting the ions as a function of the laser frequency, the energy differences between the atomic hyperfine transitions were measured.
If measurements are performed on more than one isotope, the difference in mean-square charge radius of these isotopes can be obtained from the difference in the hfs centroid frequency of two isotopes (the isotope shift) with mass numbers A and A : δν A,A = ν A − ν A .In order to apply the CRIS method to study a light element such as potassium, where the optical transition exhibits a lower sensitivity to the nuclear properties, the long-term stability and accurate measurement of the laser frequency had to be investigated.The details of the relevant developments are presented in Ref. [22], where the method was validated by measuring the mean-square charge radii of 38−47 K isotopes with high precision.For the most exotic isotope, there was an additional challenge: a large isobaric contamination at mass A = 52, measured to be 2×10 4 times more intense than the 52 K beam of interest.The resulting detected background rate was found to be an order of magnitude higher than that of the resonantly ionized 52 K ions.In addition, this background rate was found to strongly fluctuate in time, making a measurement with ion detection impossible (see the hfs spectrum in Fig. 1(a)).Taking advantage of the short half-life of 52 K (t 1/2 = 110 ms) and the fact that the isobaric contamination is largely due to the stable isotope 52 Cr, an alternative detection setup was developed, which can distinguish the stable contamination from the radioactive 52 K.A thin and a thick scintillator detector were installed behind the CRIS setup (Fig. 1).These detectors were used to count the β-particles emitted though the decay of 52 K.With this setup, the fluctuations in the background rate and signal-to-background ratio were significantly improved, as seen in Fig. 1(b).The obtained hfs spectrum of 52 K is presented in Fig. 1(c).Note that the hfs spectra of 47−51 K were re-measured with the standard CRIS method, and 50,51 K were measured with both ion-and βdetection.This allows a consistent calculation of isotope shifts of 47−52 K (See Tab II in Methods for details).
The changes in the mean-square charge radii δ r 2 are calculated from the isotope shift ν AA via Here F , K NMS and K SMS are the atomic field shift, specific mass shift and normal mass shift factors, respectively (see Methods for details).Previously published charge radii of potassium isotopes [5,18,19,21,23] have been extracted from the isotope shifts using an F -value calculated with a non-relativistic coupled-cluster method and an empirically determined K SMS value, as reported in Ref. [24].
We employ the recently developed analytic response relativistic coupled-cluster (ARRCC) theory [25], an advanced atomic many-body method (see Methods for details), to calculate both the F and K SMS constants.The newly calculated atomic field shift factor, F = −107.2(5)MHz fm 2 is in good agreement with the literature value F = −110(3) MHz fm 2 , and is more precise.More importantly, the specific mass shift, a highly correlated atomic parameter, could be calculated from microscopic atomic theory for the first time.The calculated value, K SMS = −14.0(22)GHz u, Table I.
Evaluated experimental isotope shifts δν 39,A , differences in mean-square charge radii δ r 2 , and charge radii R ch of nuclei 36−52 K. Systematic errors are reported in square brackets.The procedure for the evaluation is discussed in the Methods.
A N I π δν 39,A (MHz) δ r 2 39,A (fm 2 ) R ch (fm) 36  is more precise than the empirical value, K SMS = −15.4(38)GHz u from Ref. [24], and shows good agreement.Table I presents the isotope shifts, changes in mean-square charge radii, and absolute charge radii of 36−52 K which were extracted using these new atomic constants.The isotope shifts and charge radii have been re-evaluated using all available data, as described in the Methods section.In Fig. 2(a) these charge radii are compared with values obtained using the atomic factors taken from Ref. [24].Good agreement is obtained, while the systematic error due to the uncertainty on the atomic factors is clearly reduced.A future measurement of the absolute radii of radioactive potassium isotopes through non-optical means (e.g.electron scattering at the SCRIT facility [26]), would help reduce the systematic uncertainties.Previously, the nuclear spin and parity of 52 K was tentatively assigned to be I π = (2 − ), based on the very weak feeding into the 52 Ca ground state [27].Here, we have analysed our data assuming two other alternative spin options.Given that the I = 1 and I = 3 assumptions produce unrealistically small and large charge radii (see Fig. 2(a)), our study further supports an I = 2 assignment.
The inset in Fig. 2(a) compares the changes in meansquare charge radii (relative to the radius of isotope with neutron number N = 28) of several isotopic chains in this mass region, up to Z = 26.A remarkable observation is that the charge radii beyond N = 28 follow the same steep increasing trend, irrespective of the number of protons in the nucleus.Beyond N = 32, data are only available for potassium (this work) and manganese (Z = 25) [28].Both charge radius trends are very similar, with no signature of a characteristic kink that would indicate 'magicity' at N = 32.
Previously, ab initio coupled cluster (CC) calculations based on the NNLO sat interaction [29] were used to describe the nuclear charge radii in calcium isotopes [4,12].
At that time, calculations in this framework could only be performed for spherical isotopes near 'doubly-magic' nuclei.While these calculations predicted the absolute charge radii near 40,48 Ca very well, they failed to reproduce the observed large charge radii around neutron number N = 32.
In Fig. 2(b) we compare the experimental data to CC calculations that start from a symmetry-breaking reference state, which allows us to compute charge radii of all potassium isotopes (see Methods for details).Results obtained with the NNLO sat interaction significantly overestimate the experimental data near stability, where the experimental uncertainties on the total radii are the smallest.This interaction was fitted to experimental binding energies and charge radii of selected nuclei up to mass number A = 25 [29].Therefore, a newly constructed ∆NNLO GO (450) interaction was developed, which includes pion-physics and effects of the ∆(1232) isobar.This interaction is constrained by properties of only light nuclei with mass numbers A ≤ 4 and by nuclear matter at the saturation point (i.e. its saturation energy and density, and its symmetry energy, see Methods for details).By virtue of including saturation properties, CC calculations using the ∆NNLO GO (450) interaction yield an improvement in the accuracy of the description of potassium charge radii near stability, as shown in Fig. 2(b).
However, both NNLO sat and ∆NNLO GO (450) interactions still underestimate the steep increase observed beyond N = 28.This is better visualised by plotting the differences in meansquare charge radii relative to 47 K (with neutron number N = 28), δ r 2 47,A , shown in Fig. 2(c).The systematic uncertainties near N = 28 are strongly reduced by choosing this reference.It is also worth noting that, for δ r 2 47,A below N = 28, both interactions show a good agreement with experimental results within the systematic uncertainty.
What can be the reason for the underestimation of charge radii for N > 28?The reference state in CC calculations is the axial Hartree-Fock state.For nearly spherical nuclei, a general (triaxial) cranked HFB state that breaks time-reversal and gauge symmetries could perhaps provide a better reference.Also, since the angular momentum was not restored, the associated correlations are missing as well in CC results.
The DFT is the method of choice for heavy systems.Nuclei with Z ≈ 20 cover the region where both methods, DFT and CC, can be successfully applied.Our DFT calculations use in particular the Fayans functional Fy(∆r,HFB) [30] (see Methods for details) which was developed with a focus on charge radii.This method closely reproduces the absolute charge radii of calcium isotopes, including the steep increase beyond N = 28 [11].Furthermore, Fy(∆r,HFB) reproduces the absolute radii of the magic tin [13], cadmium [31] as well as the odd-Z copper isotopes [10].It is to be noted however, that the potassium isotopes are a lighter system in which the polarization effects are expected to be stronger than in the heavier copper isotopes.To account for that, we extended the Fayans-DFT framework to allow for deformed HFB solutions.The isotopic chain contains odd-odd nuclei and the present DFT and CC treatment does not allow a clean spin selection for these.Consequently, the HFB calculations provide an averaged description for the odd-odd isotopes.As seen in Fig. 2(b), except for the neutron-poor side, Fy(∆r,HFB) calculations reproduce the average global trend rather well, in particular the steep increase above N = 28.However, this model grossly overestimates the odd-even staggering.The odd-even staggering in the potassium isotopes is significantly reduced with respect to calcium isotopes.This is very well captured by the CC calculations, due to the fact that these describe in detail the many-body correlations (see Methods for details).In nuclear DFT, local many-body correlations are treated less precisely.
In summary, this work presents the first measurement of nuclear charge radii beyond the proposed 'magic' number N = 32 in the calcium region.This was achieved by combining collinear resonance ionization spectroscopy with β-decay detection, enabling the exotic isotope 52 K to be studied, despite its short half-life, low production rate and poor purity.Taking advantage of recent developments in atomic calculations, precise charge radii of the potassium chain were extracted.No sudden change in the 52 K charge radius is observed, thus no signature for 'magicity' at N = 32 is found.The comparison with nuclear theory predictions for the demanding case of potassium isotopes helps to uncover more about the strengths and open problems in current state-of-the-art nuclear models.CC calculations based on the new nucleon-nucleon potentials derived from chiral effective field theory, optimized with few-body nuclei properties as well as nuclear saturation properties, describe very well the absolute nuclear charge radii of the potassium isotopes near stability, and also the small odd-even staggering.However, the steep rise in charge radii above N = 28 remains underestimated.The similarity in the performance of ∆NNLO GO (450) and NNLO sat interactions suggests that the charge radii beyond N = 28 are insensitive to the details of chiral interactions at next-to-next-to-leading-order, and some crucial ingredient is lacking in these many-body methods.The Fayans-DFT model captures the general trend across the measured isotopes and reproduces the absolute radii rather well, including the steep increase up to N = 33.However, this model overestimates the odd-even staggering significantly.These findings highlight our limited understanding on the size of neutron-rich nuclei, and will undoubtedly trigger further developments in nuclear theory as demanding nuclear data on charge radii keeps uncovering problems with the best current models.

METHODS
The CRIS technique: The schematic layout of the CRIS setup is presented in Fig. 1.The mass selected ions were cooled and bunched in the ISCOOL device which operated at 100 Hz, the duty cycle of the CRIS experiment.The ion bunches typically have a 6 µs temporal width corresponding to a spatial length of around 1 m length.First, the bunched ion beam was neutralized in the CRIS beamline through collisions with potassium atoms in the charge-exchange cell (CEC).The remaining ions were deflected just after the CEC with an electrostatic deflector plate.In addition, atoms that were produced in highly excited states through the charge exchange process were field ionized and deflected out of the beam.The beam of neutral atoms passed through the differential pumping region and arrived in the 1.2-m interaction region (IR) maintained at a pressure of 10 −10 mbar.Here the atom bunch was collinearly overlapped with 3 laser pulses, which were used to stepwise excite and ionize the potassium atoms.A detailed study of this particular resonance ionization scheme can be found in Ref. [21].In the IR, ions can also be produced in non-resonant processes, introducing higher background rates [22].Normally, the ions created in the IR are guided towards an ion detector (MagneToF).This technique was used for the measurement of 47−51 K.The 51 K isotope was produced at a rate of less than 2000 particles per second and its hfs spectrum was measured in less than 2 hours.The study of 52 K, however, required a still more selective detection method.This isotope, produced at about 360 particles per second rate, is an isobar of the most abundant stable chromium isotope, which is the main contaminating species in the A = 52 beam, with an intensity of 6×10 6 particles per second.In order to avoid the detection of the non-resonantly ionized 52 Cr, the CRIS setup was equipped with a decay detection station, placed behind the end flange of the beamline.The MagneToF detector was removed from the path of the ion beam, and the ionized bunches were implanted into a thin aluminium window with 1 mm thickness allowing the transmission of β particles with energies larger than 0.6 MeV.The decay station behind this window consisted of a thin and thick scintillator detector (A and B in Fig. 1) for a coincidence detection of β-particles.The dimensions of the detectors were 1 mm × 6 cm × 6 cm and 6 cm × 6 cm × 6 cm.The β counts detected in coincidence were recorded by the data acquisition system (DAQ) together with the laser frequency detuning.The DAQ recorded the number of events in the detectors with a timestamp.The timestamp of the proton bunches impinging into the target of ISOLDE was also recorded and used to define the time gates in the data analysis.
Laser system: A three-step resonance ionization scheme was used in this experiment.
The laser light for the first excitation step was produced by a continuous wave (cw) titanium-sapphire (Ti:Sa) laser (M-Squared SolsTiS) pumped by an 18-W laser at 532 nm (Lighthouse Photonics).In order to avoid optical pumping to dark states due to long interaction times, this cw light was "chopped" into 50-ns pulses at a repetition rate of 100 Hz by using a Pockels cell [20].The wavelength of this narrowband laser was tuned to probe the hfs of the 4s 2 S 1/2 → 4p 2 P 1/2 transition at 769 nm.Atoms in the excited 4p 2 P 1/2 state were subsequently further excited to the 6s 2 S 1/2 atomic state by a pulsed dye laser (Spectron PDL SL4000) with a spectral bandwidth of 10 GHz.This dye laser was pumped by a 532 nm Nd:YAG laser (Litron TRLi 250-100) at a 100-Hz repetition rate.The fundamental output of the same Nd:YAG laser (1064 nm) was used for the final nonresonant ionization.The arrival of ion bunches and laser pulses in the interaction region were synchronized and controlled using a multi-channel pulse generator (Quantum Composers 9520 Series).

Charge radii extraction:
The perturbation of the atomic states caused by the different nuclear charge distribution in isotopes leads to small differences in the atomic transition frequency, δν AA , between centroids (ν A ,ν A ) of the hfs of two isotopes with mass number A and A .The isotope shifts of 48−52 K were extracted from the hfs spectra of 47−52 K analyzed using the SATLAS [32] Python package, as displayed in third column of Table II, along with all available results from literature.More details on the analysis process can be found in Ref. [21].The changes in the nuclear mean-square charge radii of 36−52 K can then be extracted from the isotope shifts using: where K MS and F are the atomic mass shift and field shift, m stands for the nuclear mass of isotopes A, A , and an electron.The nuclear mass was obtained by subtracting the mass of the electrons from the experimentally measured atomic mass reported in Ref. [33].The atomic constants, K MS and F , were calculated using the atomic ARRCC method as described below.The root-mean-square charge radii of these isotopes are: where R 39 is the charge radius of 39 K taken from Ref. [34].
Evaluation of the isotope shifts and charge radii: The isotope shifts of potassium isotopes were measured using several different techniques over many years, ranging from magneto-optical trap experiments [23] to laser spectroscopy of thermal [18,35,36] and accelerated beams [5,19,21], relying on photon and ion detection.The available results in Refs.[18,19,23,35,36] are referenced to the stable 39 K isotope, and are presented in the second column of Table II.The isotope shifts in Refs.[5,21] and this work, shown in the third column of Table II, were extracted with respect to 47 K.The systematic error from the experiments is given in curly brackets.Note that the systematic uncertainties in collinear laser spectroscopy experiments are mostly related to the inaccuracy of the acceleration voltage.In this work, the systematic uncertainty was negligible by using the laser scanning approach [21] and a well-calibrated high-precision voltage divider (with a relative uncertainty of 5 × 10 −5 ) from PTB.In order to compile a consistent data set with reliable evaluation of uncertainties, the following steps were taken: 1) The isotope shifts obtained with respect to 47 K were recalculated relative to 39 K, in order to link all data to the same reference.For this, the weighted average of all available δν 47,39 isotope shifts from Refs.[5,21] is used as a reference.These rereferenced values are listed in the fifth column of Table II and their uncertainty is increased due to the additional error associated with δν 39,47 (bold value in column six).Note that the systematic errors are always taken into account using the linear model [37], σ = σ sys + σ stat .
2) Next, the final isotope shift of each potassium isotope, δν 39,A (shown in the sixth column of Table II), was calculated as the weighted average (x) of the available results (x i ) using: where σ i is the total uncertainty of i th measurement.The error of the weighted mean was obtained using: accounting for possible over-, or under-dispersion using: where χ 2 is the reduced chi-squared.
3) These evaluated isotope shifts were used to extract the changes in mean-square charge radii (column 7 of Table II) using the new theoretical values for the atomic field and mass shifts, obtained in this work.
The absolute charge radii of all potassium isotopes (last column of Table II) were then calculated by using the above mentioned Eq.3, relative to the absolute radius of the stable 39 K [34].

Atomic coupled-cluster calculations:
The wave function of an atomic state with a closed-shell and a valence orbital electronic configuration can be expressed using the CC theory ansatz as where |Φ v is the mean-field wave function and S is the CC excitation operator.We further divide as S = T + S v to distinguish electron correlations without involving the valence electron (T ) and involving the valence electron (S v ).In the analytic response procedure, the first-order energy of the atomic state is obtained by solving the major harmonic oscillator shells (N max = 12) with the oscillator frequency Ω = 16 MeV.The three-body interaction has the additional cutoff on allowed threeparticle configurations This model-space is sufficient to converge the radii of all the potassium isotopes considered in this work to within ∼1% .In this work we calculate the expectation value of the squared intrinsic point proton radius, i.e.O = 1/Z i<j (r i − r j ) 2 δ tz,−1 .The coupled-cluster expectation value of the operator O is given by, is the left ground-state, and Λ is the linear combination of one-hole-one-particle and two-holetwo-particle de-excitation operators, see e.g.Ref. [39] for details.To obtain the charge radii we add finite proton/neutron, the relativistic Darwin-Foldy, and spinorbit corrections to the point proton radii.We note that the spin-orbit corrections are computed consistently as an expectation value within the CC approach, see Ref. [12].Charge radii along the chain of potassium isotopes from spherical as well as deformed calculations with the functional Fy(∆r,HFB) and compared with experimental data.
[29], which has been constrained by nucleon-nucleon properties, and binding energies and charge radii of nuclei up to oxygen.It includes terms up to next-to-nextto leading order in the Weinberg power counting.The newly constructed ∆NNLO GO (450) interaction includes ∆ isobar degrees of freedom, exhibits a cutoff of 450 MeV, and is also limited to next-to-next-to-leading order contributions.Its construction starts from the interaction of Ref. [40] and its low-energy are constrained by the saturation density, energy and symmetry energy of nuclear matter, by pion-nucleon scattering [41], nucleon-nucleon scattering, and by the A ≤ 4 nuclei.A second interaction, ∆NNLO GO (394), was similarly constructed but with a cutoff of 394 MeV.
To look at the sensitivities in the changes in the meansquare change radii, Fig. 3a compares results from the newly developed interactions with NNLO sat .While there are differences below N = 28, all interactions yield essentially identical results beyond N = 28.This suggests that charge radii beyond N = 28 are insensitive to details of chiral interactions at next-tonext-to-leading-order.
To shed more light onto this finding, Fig. 3b compares results from deformed mean-field (MF) calculations with CCSD computations for two different interactions.The 1.8/2.0(EM)interaction [42] contains contributions at next-to-next-to-next-to-leading order and thereby differs from the interactions used in this work.First, for the ∆NNLO GO (394) interaction, MF and CC yield essentially the same results for N > 28, though CC includes many more wave-function correlations.Second, for the 1.8/2.0(EM)interaction, MF and CC results differ significantly by the strong odd-even staggering, which is a correlation effect.None of the interactions explain the dramatic increase of the charge radii beyond N = 28.
DFT calculations: For the DFT part of this work, we use the non-relativistic Fayans functional in the form of Ref. [43].This functional is distinguished from other commonly used nuclear DFT in that it has additional gradient terms at two places, namely in the pairing functional and in the surface energy.The gradient terms allow, among other features, a better reproduction of the isotopic trends of charge radii [44].This motivated a refit of the Fayans functional to a broad basis of nuclear ground state data with additional information on changes in mean-square charge radii in the calcium chain [4,30].We use here Fy(∆r,HFB) from Refs.[4,30] which employed the latest data on calcium radii.It is only with rather strong gradient terms that one is able to reproduce the trends of radii in calcium at all, in particular its pronounced odd-even staggering, however, with a slight tendency to exaggerate the staggering.It was found later that Fy(∆r,HFB) performs very well in describing the trends of radii in cadmium and tin isotopes [13,31].Here we test it again for the potassium chain next to calcium.For all practical details pertaining to our Fayans-DFT calculations, we refer the reader to Ref. [30].
All above mentioned calculations with Fy(∆r,HFB) were done in spherical representation.That can be questioned for nuclei far off shell closures, the more so for odd nuclei where the odd nucleon induces a certain quadrupole moment.The new feature in the present calculations is that we use a code in axial representation which allows for deformations if the systems wants any.Fig. 2 shows the result from the deformed code [45], adapted for the Fayans functional.Here in Fig. 4 we illustrate the effect of deformation by comparison with spherical calculations.The effects are small, but show there is no uncertainty due to symmetry restrictions.The lack of angular-momentum projection in DFT calculations induces a systematic error on charge radii.We have estimated it from the angular-momentum spread to be below 0.005 fm on the average, thus having no consequences for the predicted trends.

Figure 1 .
Figure 1.Left: The CRIS setup at ISOLDE, CERN.The nuclei of interest were produced via various nuclear reactions after a 1.4-GeV proton beam impinged onto a UCx target.These diffused out of the target, into an ion source, and underwent surface ionization.The ion beam was then mass separated using a High Resolution Separator (HRS), and subsequently cooled and bunched in a linear Paul trap (ISCOOL).The bunched ion beam was guided towards the CRIS beamline, where the ions were first neutralized in a charge-exchange cell filled with potassium vapor.The neutral atoms were then delivered to the interaction region.Here the bunched beam of atoms was collinearly overlapped with the laser pulses to achieve resonance laser ionization.The ionized radioactive potassium ions could then be detected using either a MagneToF ion detector shown in (a), or plastic scintillator detectors (b).(c) The hfs of 52 K measured with the scintillator detectors.Figures (a), (b) and (c) show the detected events as a function of the laser frequency detuning.

Figure 2 .
Figure2.(a) Changes in the mean-square charge radii of potassium isotopes using the newly calculated atomic field shift (F ) and specific mass shift (KSMS) factors, as well as the values from Ref.[24].The red and gray bands indicate the uncertainties originating from these atomic constants, respectively.The inset shows the changes in the mean-square charge radii of neighbouring elements.The agreement of the data for different isotopic chains above N = 28 is striking.(b) Comparison of the measured charge radii of potassium isotopes with nuclear coupled-cluster calculations using two interactions (NNLOsat and ∆NNLOGO(450)) derived from the chiral effective field theory, and with the Fayans-DFT calculations with the Fy(∆r,HFB) energy density functional.(c) Changes in the mean-square charge radii of potassium relative to 47 K, in which the systematic uncertainties near N = 28 are largely cancelled.

Figure 3 .
Figure 3. Changes in mean-square charge radii of potassium isotopes calculated based on newly developed interactions and NNLOsat are compared with (a) experimental data and (b) that from deformed mean-field (MF) calculations with CCSD computations for two different interactions.

Figure 4 .
Figure 4.Charge radii along the chain of potassium isotopes from spherical as well as deformed calculations with the functional Fy(∆r,HFB) and compared with experimental data.
The chiral interactions we used are NNLO sat