Because of their persistent radiotoxicity, it is necessary to isolate them from humans and the biosphere and to confine them in nuclear waste repositories for geological periods of time.
As a result, the isotopic signature of the radioactivity is very different from an open air nuclear detonation where all the fission products are dispersed.
These can be recovered by nuclear reprocessing (either before or after most 137Cs and 90Sr decay) and fissioned, offering the possibility of greatly reducing waste radioactivity in the time scale of about 103 to 105 years.
On scales greater than 105 years, fission products, chiefly 99Tc, again represent a significant proportion of the remaining, though lower radioactivity, along with longer-lived actinides like neptunium-237 and plutonium-242, if those have not been destroyed.
The most abundant long-lived fission products have total decay energy around 100–300 keV, only part of which appears in the beta particle; the rest is lost to a neutrino that has no effect.
In total, the other six LLFPs, in thermal reactor spent fuel, initially release only a bit more than 10% as much energy per unit time as Tc-99 for U-235 fission, or 25% as much for 65% U-235+35% Pu-239.
99Tc is particularly attractive for transmutation not only due to the undesirable properties of the product to be destroyed and the relatively high neutron absorption cross section but also because 100Tc rapidly beta decays to stable 100Ru.