Uranium-235

Uranium-235
Uranium metal highly enriched in uranium-235
General
Symbol235U
Namesuranium-235
Protons (Z)92
Neutrons (N)143
Nuclide data
Natural abundance0.72%
Half-life (t1/2)7.04×108 years [1]
Isotope mass235.0439299 Da
Spin7/2−
Excess energy40914.062±1.970 keV
Binding energy1783870.285±1.996 keV
Parent isotopes235Pa (β)
235Np (β+)
239Pu (α)
Decay products231Th
Decay modes
Decay modeDecay energy (MeV)
Alpha4.679
Isotopes of uranium
Complete table of nuclides

Uranium-235 (235
U
or U-235) is an isotope of uranium making up about 0.72% of natural uranium. Unlike the predominant isotope uranium-238, it is fissile, i.e., it can sustain a nuclear chain reaction. It is the only fissile isotope that exists in nature as a primordial nuclide.

Uranium-235 has a half-life of 704 million years. It was discovered in 1935 by Arthur Jeffrey Dempster. Its fission cross section for slow thermal neutrons is about 584.3±1 barns.[2] For fast neutrons it is on the order of 1 barn.[3] Most neutron absorptions induce fission, though a minority (about 15%) result in the formation of uranium-236.[4][5]

  1. ^ Kondev, F. G.; Wang, M.; Huang, W. J.; Naimi, S.; Audi, G. (2021). "The NUBASE2020 evaluation of nuclear properties" (PDF). Chinese Physics C. 45 (3): 030001. doi:10.1088/1674-1137/abddae.
  2. ^ "#Standard Reaction: 235U(n,f)". www-nds.iaea.org. IAEA. Retrieved 4 May 2020.
  3. ^ ""Some Physics of Uranium", UIC.com.au". Archived from the original on July 17, 2007. Retrieved 2009-01-18.
  4. ^ "Capture-to-fission Ratio". nuclear-power.com. Retrieved June 26, 2024.
  5. ^ Cabell, M. J.; Slee, L. J. (1962). "The ratio of neutron capture to fission for uranium-235". Journal of Inorganic and Nuclear Chemistry. 24 (12): 1493–1500. doi:10.1016/0022-1902(62)80002-5.