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Splitting isotope shift in the 1s2p3P0,1,2 fine-structure triplet in C4+12,13,14: Experiment and theory

Patrick Müller1, Kristian König1,2,*, Emily Burbach1, Gordon W. F. Drake3, Phillip Imgram1, Bernhard Maass1,†, Titamarie M. Maggio3, Wilfried Nörtershäuser1,2, and Julien Spahn1

  • 1Institut für Kernphysik, Technische Universität Darmstadt, 64289 Darmstadt, Germany
  • 2Helmholtz Research Academy Hesse for FAIR, GSI Helmholtzzentrum für Schwerionenforschung, 64291 Darmstadt, Germany
  • 3Department of Physics, University of Windsor, Windsor, Ontario, Canada N9B 3P4

  • *Contact author: kkoenig@ikp.tu-darmstadt.de
  • †Current address: Physics Division, Argonne National Laboratory, 60439 Lemont, Illinois USA.

Phys. Rev. A 113, 012806 – Published 2 January, 2026

DOI: https://doi.org/10.1103/24k3-r2gp

Abstract

We report measurements and theoretical calculations of the fine-structure splittings in all three 1s2sS13→1s2pP0,1,23 transitions in the heliumlike systems of the isotopes C12,13,14. The metastable triplet state was efficiently populated in an electron beam ion source and the C4+ ions were electrostatically accelerated to 50 keV to perform collinear laser spectroscopy. From the determined transition frequencies, the splitting isotope shift (SIS), i.e., the difference in fine-structure splittings between different isotopes of the same element, was extracted. In the SIS, theoretical uncertainties due to higher-order quantum electrodynamic corrections are strongly suppressed since they are independent of both nuclear mass and the fine-structure quantum number J in lowest order. Comparison with theory provides an important test of experimental accuracy, particularly in the C4+13 case, for which the nuclear spin leads to hyperfine-induced fine-structure mixing. At the same time, the even-even isotopes C4+12,14 without nuclear spin can be used to confirm theory. Theoretical values of the SIS are given for all the heliumlike ions with 2≤Z≤10.

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