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Isotopes of Uranium
Notes
Uranium has no stable isotopes.
Notable Isotopes show graph
232U [140 neutrons]
Abundance: synthetic
Half life: 68.9 years
Decay Energy: 5.414 MeV
Decays to 228Th.
233U [141 neutrons]
Abundance: synthetic
Half life: 159200 years
Decay Energy: 4.909 MeV
Decays to 229Th.
234U [142 neutrons]
Abundance: 0.006%
Half life: 245500 years
Decay Energy: 4.859 MeV
Decays to 230Th.
235U [143 neutrons]
Abundance: 0.72%
Half life: 7.038 x 108 years
Decay Energy: 4.679 MeV
Decays to 231Th.
235U is unique in its ability to cause a rapidly expanding fission chain reaction, i.e., it is fissile. In fact, U-235 is the only fissile isotope found in nature. It was discovered in 1935 by Arthur Jeffrey Dempster. A uranium nucleus that absorbs a neutron splits into two lighter nuclei; this is called nuclear fission. It releases either two or three neutrons which continue the reaction. In nuclear reactors, the reaction is slowed down by the addition of control rods which are made of elements such as boron, cadmium, and hafnium which can absorb a large number of neutrons. In nuclear bombs, the reaction is uncontrolled and the large amount of energy released creates a nuclear explosion.
236U [144 neutrons]
Abundance: synthetic
Half life: 2.342 x 107 years
Decay Energy: 4.572 MeV
Decays to 232Th.
238U [146 neutrons]
Abundance: 99.275%
Half life: 4.468 x 109 years
Decay Energy: 4.260 MeV
Decays to 234Th.
Uranium-238 is important because it absorbs neutrons to produce a radioactive isotope that subsequently decays to the isotope plutonium-239, which is fissile, that is, can be broken apart by thermal neutrons.