Modern approach to muonic x-ray spectroscopy demonstrated through the measurement of stable Cl radii

TL;DR

This paper introduces a modern muonic x-ray spectroscopy method to measure nuclear charge radii with high precision, demonstrated through stable chlorine isotopes, and improves existing measurements significantly.

Contribution

A new experimental and computational approach for determining nuclear charge radii using muonic x-ray spectroscopy and energy density functional calculations.

Findings

Measured charge radii for $^{35}$Cl and $^{37}$Cl with improved precision.

Developed a new method for applying nuclear shape corrections from energy density functionals.

Achieved over tenfold reduction in uncertainty compared to previous electron scattering data.

Abstract

Recent advances in muonic x-ray experiments have reinvigorated efforts in measurements of absolute nuclear charge radii. Here, a modern approach is presented, and demonstrated through determination of the charge radii of the two stable chlorine nuclides $^{35}$Cl and $^{37}$Cl. Knowledge of these radii has implications for fundamental studies in nuclear and atomic physics. For this purpose, a state-of-the-art experiment was performed at the $\pi$E1 beamline in the Paul Scherrer Institute (Switzerland), using a large-scale HPGe detector array in order to extract precise energies of the muonic $^{35}$Cl and $^{37}$Cl $np1s$ transitions. The nuclear charge radius extraction relies on modern calculations for QED effects and nuclear polarization with rigorous uncertainty quantification, including effects that were not accounted for in older studies. Additionally, we established a new method for applying the nuclear shape correction directly from energy density functionals, which are amenable to isotopes for which no high-quality electron scattering experiments are available. The resulting charge radii are $3.3335(23) fm$ for $^{35}$Cl and $3.3445(23) fm$ for $^{37}$Cl, thus improving the uncertainty of the available electron scattering values by a factor of seven. The correlation of several observables was evaluated between the different isotopes in order to produce a more precise value of the differential mean square charge radius $\delta \langle r^2 \rangle^{37, 35}=+0.0771(66) fm^{2}$. In this case, improvement of the uncertainty by more than one order of magnitude was achieved compared to the literature value. This precision is sufficient to use this differential as input for isotope shift factor determination.