As shown in figure
2, the slopes of the rms charge radii as a function of neutron number are similar in the neutron range
N = 126 − 138. The rapid increases in rms charge radii can be found remarkably across the neutron number
N = 138 along polonium, thorium, plutonium, and curium isotopic chains. Actually, this scenario can also be found in radon and radium isotopes but with small amplitudes. As mentioned in [
98], the different sequences of the occupation of the single-particle levels lead to changes of charge radii. In which the subshell 1
i11/2 is completely filled (
N = 138) and then the added neutron will be filled in subshell 2
g9/2 up to
N = 148. In our calculations, the calculated quadrupole deformations along even
Z = 84 − 96 isotopic chains are almost spherical from
N = 126 to
N = 138. Across
N = 138 subshell, the rapid raise in rms charge radii attributes to the increasing deformation parameter, namely
β20 > 0.20. In uranium isotopes, the jump in charge radii disappeared due to the calculated values of
β20 are almost close to zero from
N = 121 − 147. Across the
N = 148, the rapid change of the rms charge radius can also be observed evidently in uranium isotopes, in which the deformation parameter
β20 equals to 0.30.