Category
page 1Uranium
uranium
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
depleted uranium
uranium with a lower content of the fissile isotope U-235 than natural uranium
enriched uranium
uranium in which the proportion of uranium-235 has been increased through the process of isotope separation
uranium-238
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
Oak Ridge National Laboratory
government research facility in Tennessee, United States
uranium glass
glass colored with uranium oxide

calutron
thumb|alt=A man stands in front of a C-shaped object twice his size.|An Alpha calutron tank removed from the magnet for recovery of uranium-235
thumb|alt=A large oval-shaped structure|Alpha I magnet, called the "Racetrack". The calutrons are located around the ring.
isotope of uranium
nuclides with atomic number Z = 92 and with different mass numbers
Gaseous diffusion
Nuclear Economy Process
uranium-thorium dating
radiometric dating method based on the degree to which secular equilibrium has been achieved between the parent U-234 and the daughter Th-230
natural nuclear fission reactor
naturally occurring uranium deposit where self-sustaining nuclear chain reactions have occurred
gas centrifuge
device for chemical separation
Q903801
French chemist (1811–1890)
PUREX
thumb|upright=1.1|Reprocessing of spent nuclear fuel by the PUREX method, first developed in the 1940s to produce plutonium for nuclear weapons, was demonstrated commercially in Belgium to partially re-fuel a LWR in the 1960s. This aqueous chemical process continues to be used commercially to separate [[reactor grade plutonium (RGPu) for reuse as MOX fuel. It remains controversial, as plutonium can be used to make nuclear weapons.]]
uranium ore
economically recoverable concentrations of uranium within the Earth's crust
natural uranium
uranium with the same isotopic ratio as found in nature
Atomic vapor laser isotope separation
Method of separating isotopes of uranium
fission track dating
radiometric dating technique based on analyses of the damage trails, or tracks, left by fission fragments in certain uranium-bearing minerals and glasses
Uranium hydride bomb
type of atom bomb
in situ leach mining
mining through artificially dissolving minerals in a borehole
Uranium in the environment

blanket
technical term
reprocessed uranium
uranium recovered from nuclear fuel reprocessing
pleochroic halo
Geological phenomenon
weapons-grade
substance that is pure enough to be used to make a weapon