Periodic Table

Uranium

Actinide

Quick Facts about Uranium

Pa
  • solid- state of matter at room temperature
  • Radioactive- no stable isotopes exist
  • +6, +5, +4, +3- common oxidation states in compounds
  • ORC- crystal structure, atomic arrangement in solid form
Np

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.

Why Uranium Matters

The element that powers cities and changed world history forever

In Your Home

  • Uranium glass (antique glassware glows green)
  • Smoke detectors use americium (made from uranium)
  • Some ceramic glazes (historical)
  • Depleted uranium counterweights (aircraft)

Industry Uses

EnergyNuclear power plants generate 10% of world electricity
MilitaryNuclear weapons and depleted uranium ammunition
MedicalProduces isotopes for medical imaging
ResearchFundamental physics research

In Your Body

✗ Not essential

No biological function. Chemically toxic to kidneys (heavy metal). Radiation from enriched uranium is also dangerous.

Safety: Both chemically toxic and radioactive. Natural uranium's radioactivity is relatively low. Kidney damage is primary concern.

Discovery of Uranium

Discovered by Martin Klaproth in Germany, 1789

Name origin: Named for the planet Uranus.

History & Events

1789
Discovery
Martin Heinrich Klaproth discovered uranium in pitchblende, named for planet Uranus
1942
First Chain Reaction
Enrico Fermi achieved first controlled nuclear reaction at University of Chicago
1945
Atomic Bombs
US dropped uranium and plutonium bombs on Hiroshima and Nagasaki

About Uranium

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.

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

Physical Properties of U

Phase (STP)
solid
Melting Point of U
1405.30 K
Boiling Point of U
4404.00 K
Density of U
19.1000 g/cm3

Thermal Properties

Heat of Fusion
12.60 kJ/mol
Heat of Vaporization
417.00 kJ/mol
Specific Heat
0.12 J/g·K
Molar Heat Capacity
27.66 J/mol·K
Thermal Conductivity
27.50 W/m·K

Atomic Radii

Calculated
175 pm
Covalent
170 pm
Van der Waals
241 pm

Common Misconceptions

Wrong:All uranium is weapons-grade.
Correct:Natural uranium is 0.7% U-235. Weapons need 90%+ enrichment. Reactor fuel uses 3-5%.
Wrong:Uranium is extremely rare.
Correct:Uranium is more common than tin in Earth's crust. Economically recoverable deposits are limited.
Wrong:Nuclear power always leads to weapons.
Correct:Commercial reactor uranium (3-5% U-235) cannot be used for weapons without extensive enrichment.

Isotopes of Uranium

Uranium has 0 naturally occurring isotopes, plus 6 notable radioactive isotopes.

IsotopeAtomic Mass (u)AbundanceHalf-LifeDecay Mode
23392U (U-233)Uranium-233 isotope233.0396355
23492U (U-234)Uranium-234 isotope234.04095235.40×10-3%245,500 yearsα
23592U (U-235)Uranium-235 isotope235.04393010.7204%703.8 million yearsα
23692U (U-236)Uranium-236 isotope236.045568223.42 million yearsα
23892U (U-238)Uranium-238 isotope238.050788499.27%4.468 billion yearsα
23992U (U-239)Uranium-239 isotope239.05429350%23.45 minutesβ⁻

Data source: NIH PubChem (aggregated from IUPAC, NIST)

Isotope Applications

Selected uses of notable Uranium isotopes.

U-235

Fissile isotope used as fuel in nuclear reactors; the only naturally occurring fissile nuclide present in appreciable quantity

U-238

Parent isotope for U-decay series; source of fissile Pu-239 via neutron capture

U-239

Short-lived intermediate in the production chain from uranium-238 to plutonium-239

Applications reference: IUPAC Isotopes Matter and NIH PubChem.

Abundance

Earth's Crust
2.7 mg/kg
Seawater
3.20 μg/kg

Uses

For many centuries it was used as a pigment for glass. Now it is used as a fuel in nuclear reactors and in bombs.

Occurrence and Production

Occurs in many rocks, but in large amounts only in such minerals as pitchblende and carnotite.

Geochemistry

Goldschmidt
litophile
Geochemical Class
rare earth & related

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