Uranium-232 () is an isotope of uranium. It has a half-life of 68.9 years and is a side product in the thorium cycle. It has been cited as an obstacle to nuclear proliferation using <sup>233</sup>U as the fissile material, because the intense gamma radiation emitted by <sup>208</sup>Tl (a daughter of <sup>232</sup>U, produced relatively quickly) makes the <sup>233</sup>U contaminated with it more difficult to handle.
Production of <sup>233</sup>U (through the neutron irradiation of <sup>232</sup>Th) invariably produces small amounts of <sup>232</sup>U as an impurity, because of parasitic (n,2n) reactions on uranium-233 itself, or on protactinium-233, or on thorium-232:
Another channel involves neutron capture reaction on small amounts of thorium-230, which is a tiny fraction of natural thorium present due to the decay of uranium-238:
The decay chain of <sup>232</sup>U quickly yields strong gamma radiation emitters:
This makes manual handling in a glove box with only light shielding (as commonly done with plutonium) too hazardous, except in a period short compared to the Th-228 half-life just after chemical separation of the uranium, and instead requiring remote manipulation for fuel fabrication.
Unusually for an isotope with even mass number, <sup>232</sup>U has a significant neutron absorption cross section for fission (thermal neutrons , resonance integral ) as well as for neutron capture (thermal , resonance integral ). This makes it a fissile isotope, though using it alone in a reactor or bomb is not reasonable.