Uranium-235
Uranium metal highly enriched in uranium-235 | |
| General | |
|---|---|
| Symbol | 235U |
| Names | uranium-235 |
| Protons (Z) | 92 |
| Neutrons (N) | 143 |
| Nuclide data | |
| Natural abundance | 0.72% |
| Half-life (t1/2) | 7.04×108 years |
| Isotope mass | 235.043928 Da |
| Spin | 7/2− |
| Excess energy | 40914.062±1.970 keV |
| Nuclear binding energy | 1783870.285±1.996 keV |
| Parent isotopes | 235Pa (β−) 235Np (β+) 239Pu (α) |
| Decay products | 231Th |
| Decay modes | |
| Decay mode | Decay energy (MeV) |
| Alpha | 4.679 |
| Isotopes of uranium Complete table of nuclides | |
Uranium-235 (235
U or U-235) is an isotope of uranium making up about 0.72% of natural uranium. Unlike the predominant isotope uranium-238, it is fissile, i.e., it can sustain a nuclear chain reaction. It is the only fissile isotope that exists in nature as a primordial nuclide.
Uranium-235 has a half-life of 704 million years. It was discovered in 1935 by Arthur Jeffrey Dempster. Its fission cross section for slow thermal neutrons is about 584.3±1 barns. For fast neutrons it is on the order of 1 barn. Most neutron absorptions induce fission, though a minority (about 15%) result in the formation of uranium-236.