Atomic Properties of U
- Atomic Number of U
- 92
- Atomic Mass of U
- 238.0300 u
- Electron Configuration
- [Rn] 5f3 6d1 7s2
- Electronegativity
- 1.38
- Block
- f-block
- Group
- —
- Period
- 7
Uranium (U) is element 92 on the periodic table. Atomic mass of U: 238.0300 u. U is in period 7. Melting point of U: 1405.30 K.Density of U: 19.10 g/cm³.
The element that powers cities and changed world history forever
No biological function. Chemically toxic to kidneys (heavy metal). Radiation from enriched uranium is also dangerous.
Discovered by Martin Klaproth in Germany, 1789
Name origin: Named for the planet Uranus.
White radioactive metallic element belonging to the actinoids. Three natural isotopes, U-238, U-235 and U-234. Uranium-235 is used as the fuel for nuclear reactors and weapons. Discovered by Martin H. Klaproth in 1789.
Uranium has 0 naturally occurring isotopes, plus 6 notable radioactive isotopes.
| Isotope | Atomic Mass (u) | Abundance | Half-Life | Decay Mode |
|---|---|---|---|---|
| 23392U (U-233)Uranium-233 isotope | 233.0396355 | — | — | — |
| 23492U (U-234)Uranium-234 isotope | 234.0409523 | 5.40×10-3% | 245,500 years | α |
| 23592U (U-235)Uranium-235 isotope | 235.0439301 | 0.7204% | 703.8 million years | α |
| 23692U (U-236)Uranium-236 isotope | 236.0455682 | — | 23.42 million years | α |
| 23892U (U-238)Uranium-238 isotope | 238.0507884 | 99.27% | 4.468 billion years | α |
| 23992U (U-239)Uranium-239 isotope | 239.0542935 | 0% | 23.45 minutes | β⁻ |
Data source: NIH PubChem (aggregated from IUPAC, NIST)
Selected uses of notable Uranium isotopes.
Fissile isotope used as fuel in nuclear reactors; the only naturally occurring fissile nuclide present in appreciable quantity
Parent isotope for U-decay series; source of fissile Pu-239 via neutron capture
Short-lived intermediate in the production chain from uranium-238 to plutonium-239
Applications reference: IUPAC Isotopes Matter and NIH PubChem.
For many centuries it was used as a pigment for glass. Now it is used as a fuel in nuclear reactors and in bombs.
Occurs in many rocks, but in large amounts only in such minerals as pitchblende and carnotite.
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The chemistry behind Uranium: