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uranium-238

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Also known as 238U, U-238, ²³⁸U

Uranium-238 (' or U-238') is the most common isotope of uranium found in nature, with a relative abundance above 99%. Unlike uranium-235, it is non-fissile, which means it cannot sustain a chain reaction in a thermal-neutron reactor. However, it is fissionable by fast neutrons, and is fertile, meaning it can be transmuted to fissile plutonium-239. 238U cannot support a chain reaction because inelastic scattering reduces neutron energy below the range where fast fission of one or more next-generation nuclei is probable. Doppler broadening of 238U's neutron absorption resonances, increasing abso

Key facts

Isotope.image
Uranium03.jpg
Isotope.image_caption
10-gram sample
Isotope.mass_number
238
Isotope.symbol
U
Isotope.num_neutrons
146
Isotope.num_protons
92
Isotope.abundance
99.274%
Isotope.decay_product
Thorium-234
Isotope.decay_mass
234
Isotope.decay_symbol
Th
Isotope.parent
Plutonium-242
Isotope.parent_mass
242
Isotope.parent_symbol
Pu
Isotope.parent_decay
a
Isotope.parent2
Protactinium-238
Isotope.parent2_mass
238
Isotope.parent2_symbol
Pa
Isotope.parent2_decay
b-

via Wikipedia infobox

Wikidata facts

Mass
238.050786996
Image
Uranium238.jpg
Show 9 more facts
atomic number
92
neutron number
146
half-life
4468000000
natural abundance
0.992742
spin quantum number
0.0
parity quantum number
1
mass excess
47307.783
binding energy
1801689.75
Commons category
Uranium-238
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via Wikidata · CC0

~14 min read

Article

12 sections
Contents
  • Nuclear energy applications
  • Breeder reactors
  • CANDU reactors
  • Radiation shielding
  • Downblending
  • Nuclear weapons
  • Decay
  • Radioactive dating
  • Health concerns
  • See also
  • References
  • External links

Uranium-238 (' or U-238') is the most common isotope of uranium found in nature, with a relative abundance above 99%. Unlike uranium-235, it is non-fissile, which means it cannot sustain a chain reaction in a thermal-neutron reactor. However, it is fissionable by fast neutrons, and is fertile, meaning it can be transmuted to fissile plutonium-239. 238U cannot support a chain reaction because inelastic scattering reduces neutron energy below the range where fast fission of one or more next-generation nuclei is probable. Doppler broadening of 238U's neutron absorption resonances, increasing absorption as fuel temperature increases, is also an essential negative feedback mechanism for reactor control.

The isotope has a half-life of 4.463 billion years (). Due to its abundance and half-life relative rate of decay to other radioactive elements, 238U is responsible for about 40% of the radioactive heat produced within the Earth. The 238U decay chain contributes six electron anti-neutrinos per 238U nucleus (one per beta decay), resulting in a large detectable geoneutrino signal when decays occur within the Earth. The decay of 238U to daughter isotopes is extensively used in radiometric dating, particularly for material older than approximately 1 million years.

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