Uranium-243 is a radioisotope of the chemical element uranium, which, in addition to the element-specific 92 protons, has 151 neutrons in the atomic nucleus, resulting in the mass number 243. The very short-lived, only artificially producible, unstable and therefore radioactive nuclide has no practical significance; dealing with 243U is for academic purposes only.
The nuclide was indirectly detected in the fallout of the thermonuclear test (Ivy Mike) on November 1, 1952 in the Pacific Ocean [1]; there is no confirmation to date. The data given here are theoretical or estimated.
See also: List of individual Uranium isotopes (and general data sources).
Half-life T½ = 10 s respectively 1 × 101 seconds s.
| Decay mode | Daughter | Probability | Decay energy | γ energy (intensity) |
|---|---|---|---|---|
| β- | 243Np | ? | 2.67 MeV |
| Z | Isotone N = 151 | Isobar A = 243 |
|---|---|---|
| 92 | 243U | 243U |
| 93 | 244Np | 243Np |
| 94 | 245Pu | 243Pu |
| 95 | 246Am | 243Am |
| 96 | 247Cm | 243Cm |
| 97 | 248Bk | 243Bk |
| 98 | 249Cf | 243Cf |
| 99 | 250Es | 243Es |
| 100 | 251Fm | 243Fm |
| 101 | 252Md | |
| 102 | 253No | |
| 103 | 254Lr | |
| 104 | 255Rf | |
| 105 | 256Db | |
| 106 | 257Sg |
[1] - H. Diamond, P. R. Fields, C. S. Stevens et al.:
Heavy Isotope Abundances in Mike Thermonuclear Device.
In: Physical Review, 119, 2000, (1960), DOI 10.1103/PhysRev.119.2000.
Last update: 2024-08-28
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