Uranium-235
Uranium-235 (235U 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 metal highly enriched in uranium-235 | |
| General | |
|---|---|
| Symbol | 235U |
| Names | uranium-235, 235U, U-235 |
| Protons (Z) | 92 |
| Neutrons (N) | 143 |
| Nuclide data | |
| Natural abundance | 0.72% |
| Half-life (t1/2) | 703800000 years |
| Isotope mass | 235.0439299 Da |
| Spin | 7/2− |
| Excess energy | 40914.062±1.970 keV |
| Binding energy | 1783870.285±1.996 keV |
| Parent isotopes | 235Pa 235Np 239Pu |
| Decay products | 231Th |
| Decay modes | |
| Decay mode | Decay energy (MeV) |
| Alpha | 4.679 |
| Isotopes of uranium Complete table of nuclides | |
Uranium-235 has a half-life of 703.8 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 result in the formation of uranium-236.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.