Skip to content
uranium

File:HEUraniumC.jpg · Wikimedia Commons · See Wikimedia Commons

EntityQ1098· pop 175· linked from 3,937 articles

Also known as element 92, U

Uranium is a chemical element; it has symbol U and atomic number 92. It is a silvery-grey metal in the actinide series of the periodic table. A uranium atom has 92 protons and 92 electrons, of which 6 are valence electrons. Uranium radioactively decays, usually by emitting an alpha particle. The half-life of this decay varies between 159,200 and 4.5 billion years for different isotopes, making them useful for dating the age of the Earth. The most common isotopes in natural uranium are uranium-238 (which has 146 neutrons and accounts for over 99% of uranium on Earth) and uranium-235 (which

OverviewAI-generated

Uranium is a chemical element with the symbol U and atomic number 92. It has a mass of 238.02891 and a density of 19.05. The element was discovered in 1789. Its chemical formula is U, and it has an electronegativity of 1.38. The ionic radius is 1.17.

The IUPAC name for the element is uranium. It has a charge of 0 and a TPSA of 0. There are no hydrogen bond donors or acceptors. The canonical SMILES representation is [U]. The Unicode character for the element is 鈾. Other symbols include Ur.

Research on uranium is documented in PubMed, with a count of 16387. The PubChem CID is 23989. The InChIKey is JFALSRSLKYAFGM-UHFFFAOYSA-N. The element is referenced by 3,937 other encyclopedia articles.

Synthesized by Vinony from 24 facts across 4 sources: Wikidata, PubChem, PubMed, Vinony graph. Generated from structured data (not the Wikipedia text) and checked against those facts — may still contain errors.

Chemical data

Formula
U
Molecular weight
238.0289 g/mol
IUPAC name
uranium
SMILES
[U]
InChIKey
JFALSRSLKYAFGM-UHFFFAOYSA-N
Polar surface area
0 Ų
H-bond donors
0
H-bond acceptors
0
Formal charge
0

via PubChem

Research

16,387 papers

via PubMed

~58 min read

Encyclopedic overview

35 sections
Contents
  • Characteristics
  • Applications
  • Military
  • Civilian
  • History
  • Pre-discovery use
  • Discovery
  • Fission research
  • Nuclear weaponry
  • Reactors
  • Prehistoric naturally occurring fission
  • Contamination and the Cold War legacy
  • Occurrence
  • Origin
  • Biotic and abiotic
  • Production and mining
  • Resources and reserves
  • Supplies
  • Compounds
  • Oxidation states and oxides
  • Oxides
  • Aqueous chemistry
  • Carbonates
  • Effects of pH
  • Hydrides, carbides and nitrides
  • Halides
  • Isotopes
  • Enrichment
  • Human exposure
  • Effects and precautions
  • See also
  • Notes
  • References
  • Sources cited
  • External links

Uranium is a chemical element; it has symbol U and atomic number 92. It is a silvery-grey metal in the actinide series of the periodic table. A uranium atom has 92 protons and 92 electrons, of which 6 are valence electrons. Uranium radioactively decays, usually by emitting an alpha particle. The half-life of this decay varies between 159,200 and 4.5 billion years for different isotopes, making them useful for dating the age of the Earth. The most common isotopes in natural uranium are uranium-238 (which has 146 neutrons and accounts for over 99% of uranium on Earth) and uranium-235 (which has 143 neutrons). Uranium has the highest atomic weight of the primordially occurring elements. Its density is about 70% higher than that of lead and slightly lower than that of gold or tungsten. It occurs naturally in low concentrations of a few parts per million in soil, rock and water, and is commercially extracted from uranium-bearing minerals such as uraninite.

Many contemporary uses of uranium exploit its unique nuclear properties. Uranium is used in nuclear power plants and nuclear weapons because it is the only naturally occurring element with a fissile isotope – uranium-235 – present in non-trace amounts. However, because of the low abundance of uranium-235 in natural uranium (which is overwhelmingly uranium-238), uranium needs to undergo enrichment so that enough uranium-235 is present. Uranium-238 is fissionable by fast neutrons and is fertile, meaning it can be transmuted to fissile plutonium-239 in a nuclear reactor. Another fissile isotope, uranium-233, can be produced from natural thorium and is studied for future industrial use in nuclear technology. Uranium-238 has a small probability for spontaneous fission or even induced fission with fast neutrons; uranium-235, and to a lesser degree uranium-233, have a much higher fission cross-section for slow neutrons. In sufficient concentration, these isotopes maintain a sustained nuclear chain reaction. This generates the heat in nuclear power reactors and produces the fissile material for nuclear weapons. The primary civilian use for uranium harnesses the heat energy to produce electricity. Depleted uranium (U) is used in kinetic energy penetrators and armor plating.

Excerpted from Wikipedia’s “uranium” article, available under the CC BY-SA 4.0 licence.

Gallery (53)