Ions generally do not have a measurably different rate of radioactive decay compared to their neutral counterparts, except in cases of isotopes that decay solely by electron capture. For these isotopes, complete ionization (removal of all electrons) can prevent decay entirely. When discussing half-lives, it's important to note that each isotope of an element has its own distinct half-life, which can vary significantly. For example, isotopes of gold exhibit different decay modes and half-lives. Additionally, electronic configurations can slightly influence transition energies in certain nuclei, potentially affecting their lifetimes. Overall, isotopes are defined by differing neutron counts, and not all isotopes are radioactive, with some being stable.