General | |
---|---|
Symbol | ^{234}U |
Names | uranium-234, U-234 |
Protons | 92 |
Neutrons | 142 |
Nuclide data | |
Natural abundance | 0.0054% |
Half-life | |
Parent isotopes | ^{238}U (alpha, beta, beta) ^{234}Pa (β^{-}) ^{238}Pu (α) |
Decay products | ^{230}Th |
Decay modes | |
Decay mode | Decay energy (MeV) |
alpha emission | 4.8 |
Isotopes of uranium Complete table of nuclides |
Uranium-234 (^{234}U) is an isotope of uranium. In natural uranium and in uranium ore, U-234 occurs as an indirect decay product of uranium-238, but it makes up only 0.0055% (55 parts per million) of the raw uranium because its half-life of just 245,500 years is only about 1/18,000 as long as that of U-238. The primary path of production of U-234 via nuclear decay is as follows: U-238 nuclei emit an alpha particle to become thorium-234 (Th-234). Next, with a short half-life, Th-234 nuclei emit a beta particle to become protactinium-234 (Pa-234), or more likely a nuclear isomer denoted Pa-234m. Finally, Pa-234 or Pa-234m nuclei emit another beta particle to become U-234 nuclei.
U-234 nuclei decay by alpha emission to thorium-230, except for the tiny fraction (parts per billion) of nuclei which undergo spontaneous fission.
Extraction of rather small amounts of U-234 from natural uranium would be feasible using isotope separation, similar to that used for regular uranium-enrichment. However, there is no real demand in chemistry, physics, or engineering for isolating U-234. Very small pure samples of U-234 can be extracted via the chemical ion-exchange process - from samples of plutonium-238 that have been aged somewhat to allow some decay to U-234 via alpha emission.
Enriched uranium contains more U-234 than natural uranium as a byproduct of the uranium enrichment process aimed at obtaining U-235, which concentrates lighter isotopes even more strongly than it does U-235. The increased percentage of U-234 in enriched natural uranium is acceptable in current nuclear reactors, but (re-enriched) reprocessed uranium might contain even higher fractions of U-234, which is undesirable. This is because U-234 is not fissile, and tends to absorb slow neutrons in a nuclear reactor - becoming U-235.
U-234 has a neutron-capture cross section of about 100 barns for thermal neutrons, and about 700 barns for its resonance integral - the average over neutrons having various intermediate energies. In a nuclear reactor non-fissile isotopes capture a neutron breeding fissile isotopes. U-234 is converted to U-235 more easily and therefore at a greater rate than U-238 is to Pu-239 (via neptunium-239) because U-238 has a much smaller neutron-capture cross-section of just 2.7 barns.
However, (n, 2n) reactions with fast neutrons also convert small amounts of U-235 to U-234, so that spent nuclear fuel may contain about 0.010% U-234, a much higher fraction than in non-irradiated uranium.^{[1]}
Depleted uranium contains much less U-234 (around 0.001%^{[2]}) which makes the radioactivity of depleted uranium about one-half of that of natural uranium. Natural uranium has an "equilibrium" concentration of U-234 at the point where an equal number of decays of U-238 and U-234 will occur.
Lighter: uranium-233 |
Uranium-234 is an isotope of uranium |
Heavier: uranium-235 |
Decay product of: plutonium-238 (?) protactinium-234 (?-) neptunium-234 (?+) |
Decay chain of uranium-234 |
Decays to: thorium-230 (?) |