“…After selective ionization, the ions were accelerated by a 30-kV electrostatic potential, and mass separated according to their mass-to-charge ratio using the General Purpose Separator (GPS). The pure ion beam of the isotope of interest was then transported either to the Windmill (WM) decay station [27] or the ISOLTRAP Multi-Reflection Time-of-flight Mass Spectrometer (MR-ToF MS) [17,28]. The WM detection system was utilized for detailed αand β-decay studies of 180 Au, while both setups were used for taking hfs scans for 180,182 Au, either via α-decay tagging in the case of the WM or photo-ion counting using the high-resolution mass-selective MR-ToF MS, see Refs.…”