“…Significantly higher exposures (a factor of 10 3 − 10 4 ) of these leading experiments, as well as their underground location and well-shielded low-background set-ups were the major factors of such enhanced sensitivity, as shown in table 7. It should be also stressed that only a dozen nuclei among potentially 2𝜀, 𝜀𝛽 + , 2𝛽 + active isotopes were investigated at the level of sensitivity around or more than 10 21 yr, such as 36 Ar, 40 Ca, 58 Ni, 64 Zn, 78 Kr, 96 Ru, 106 Cd, 112 Sn, 124 Xe, 130 Ba, 132 Ba, see [94] and references therein. The current limitation of the experimental sensitivity in these studies is a consequence of few reasons: a) lower energy releases in 2𝜀, 𝜀𝛽 + , 2𝛽 + processes in comparison to those in 2𝛽 − decay, that complicates background suppression; b) higher expected 𝑇 1/2 values, as a result of low decay energies and phase space factors; and c) lower natural isotopic abundances of these isotopes (typically less than 1% with only few exceptions).…”