U, element 92, density 19 g/cm3, melting point 1132°C. The heaviest of the naturally occurring elements, it has no stable isotopes, but the commonest (238U) has a half-life of more than 109 years. Once used as a yellow glass pigment, uranium compounds are now used almost exclusively for conversion to plutonium in nuclear fuel applications.
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| Name, Symbol, Number | uranium, U, 92 | ||||||||||||||||||||||||||||||||||||||||||
| Chemical series | actinides | ||||||||||||||||||||||||||||||||||||||||||
| Group, Period, Block | n/a, 7, f | ||||||||||||||||||||||||||||||||||||||||||
| Appearance |
silvery gray metallic; corrodes to a spalling black oxide coat in air |
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| Atomic mass | 238.02891(3) g/mol | ||||||||||||||||||||||||||||||||||||||||||
| Electron configuration | [Rn] 5f 7s2 | ||||||||||||||||||||||||||||||||||||||||||
| Electrons per shell | 2, 8, 18, 32, 21, 9, 2 | ||||||||||||||||||||||||||||||||||||||||||
| Physical properties | |||||||||||||||||||||||||||||||||||||||||||
| Phase | solid | ||||||||||||||||||||||||||||||||||||||||||
| Density (near r.t.) | 19.1 g·cm−3 | ||||||||||||||||||||||||||||||||||||||||||
| Liquid density at m.p. | 17.3 g·cm−3 | ||||||||||||||||||||||||||||||||||||||||||
| Melting point |
1405.3 K (1132.2 °C, 2070 °F) |
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| Boiling point |
4404 K (4131 °C, 7468 °F) |
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| Heat of fusion | 9.14 kJ·mol−1 | ||||||||||||||||||||||||||||||||||||||||||
| Heat of vaporization | 417.1 kJ·mol−1 | ||||||||||||||||||||||||||||||||||||||||||
| Heat capacity | (25 °C) 27.665 J·mol | ||||||||||||||||||||||||||||||||||||||||||
Vapor pressure
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| Atomic properties | |||||||||||||||||||||||||||||||||||||||||||
| Crystal structure | orthorhombic | ||||||||||||||||||||||||||||||||||||||||||
| Oxidation states |
3+,4+,5+,6+ (weakly basic oxide) |
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| Electronegativity | 1.38 (Pauling scale) | ||||||||||||||||||||||||||||||||||||||||||
| Ionization energies | 1st: 597.6 kJ/mol | ||||||||||||||||||||||||||||||||||||||||||
| 2nd: 1420 kJ/mol | |||||||||||||||||||||||||||||||||||||||||||
| Atomic radius | 175 pm | ||||||||||||||||||||||||||||||||||||||||||
| Van der Waals radius | 186 pm | ||||||||||||||||||||||||||||||||||||||||||
| Miscellaneous | |||||||||||||||||||||||||||||||||||||||||||
| Magnetic ordering | paramagnetic | ||||||||||||||||||||||||||||||||||||||||||
| Electrical resistivity | (0 °C) 0.280 µΩ·m | ||||||||||||||||||||||||||||||||||||||||||
| Thermal conductivity | (300 K) 27.5 W·m | ||||||||||||||||||||||||||||||||||||||||||
| Thermal expansion | (25 °C) 13.9 µm·m | ||||||||||||||||||||||||||||||||||||||||||
| Speed of sound (thin rod) | (20 °C) 3155 m/s | ||||||||||||||||||||||||||||||||||||||||||
| Young's modulus | 208 GPa | ||||||||||||||||||||||||||||||||||||||||||
| Shear modulus | 111 GPa | ||||||||||||||||||||||||||||||||||||||||||
| Bulk modulus | 100 GPa | ||||||||||||||||||||||||||||||||||||||||||
| Poisson ratio | 0.23 | ||||||||||||||||||||||||||||||||||||||||||
| CAS registry number | 7440-61-1 | ||||||||||||||||||||||||||||||||||||||||||
| Selected isotopes | |||||||||||||||||||||||||||||||||||||||||||
Main article: Isotopes of uranium
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Applications
Before radiation was discovered, uranium was primarily used in small amounts for yellow glass and pottery dyes (such as uranium glass and in Fiestaware.) There was also some use in photographic chemicals (esp. Generally this is in the form of enriched uranium, which has been processed to have higher-than-natural levels of U, though some reactor designs (such as the Candu reactors) can use natural uranium (unenriched, less than 1% U (the exact values are classified information). Depleted uranium (uranium with the percentage of 235U lowered to 0.2%) has found use as counterweights for aircraft control surfaces, as ballast for missile re-entry vehicles and as a shielding material.
History
The use of uranium, in its natural oxide form, dates back to at least CE 79, when it was used to add a yellow color to ceramic glazes (yellow glass with 1% uranium oxide was found near Naples, Italy). Uranium was found to be radioactive by French physicist Henri Becquerel in 1896, who first discovered the process of radioactivity with uranium minerals. Initially it was believed that uranium was relatively rare, and that nuclear proliferation could be avoided by simply buying up all known uranium stocks, though within a decade large deposits of it were discovered in many places around the world.
During the Manhattan Project, the names tuballoy and oralloy were used to refer to natural uranium and enriched uranium respectively, originally for purposes of secrecy.
Uranium ore is rock containing uranium mineralisation in concentrations that can be mined economically, typically 1 to 4 pounds of uranium oxide per ton or 0.05 to 0.20 percent uranium oxide.
Production and distribution
Commercial-grade uranium can be produced through the reduction of uranium halides with alkali or alkaline earth metals.
Uranium exploration and mining
Uranium is distributed worldwide. Almost all the uranium is exported, but under strict International Atomic Energy Agency safeguards to satisfy the Australian people and government that none of the uranium is used in nuclear weapons. Cameco, the world’s largest, low-cost uranium producer accounting for 18% of the world’s uranium production, operates three mines in the area.
Compounds
Uranium tetrafluoride (UF4) is known as "green salt" and is an intermediate product in the production of uranium hexafluoride.
Uranium carbonate (UO2(CO3)) is found in both the mineral and organic fractions of coal and its fly ash and is the main component of uranium in mine tailing seepage water. The process produces huge quantities of uranium that is depleted of U, called depleted uranium or "DU". From Pressurised water reactors (PWRs) of typical design (most USA reactors are PWR) we note the fuel goes in with about 4% U and comes out with about 1% Pu and 95% Pu were removed (fuel reprocessing is not allowed in the USA) and this were added to the depleted uranium then we would have 1.2% fissile material in the reprocessed depleted uranium and at the same time have 1% fissile material in the left over spent fuel. Although accidental inhalation exposure to a high concentration of uranium hexafluoride has resulted in human fatalities, those deaths were not associated with uranium . On the basis of the available data, exposure to environmental uranium or to uranium at levels found at hazardous waste sites will not be lethal to humans. Uranyl (UO2+) ions, such as from uranium trioxide or uranyl nitrate and other hexavalent uranium compounds have been shown to cause birth defects and immune system damage in laboratory animals.
Finely-divided uranium metal presents a fire hazard because uranium is pyrophoric, so small grains will ignite spontaneously in air at room temperature. however, people who live near government facilities that made or tested nuclear weapons, or facilities that mine or process uranium ore or enrich uranium for reactor fuel, may have increased exposure to uranium. Uranium does not absorb through the skin, and alpha particles released by uranium cannot penetrate the skin, so uranium that is outside the body is much less harmful than it would be if it were inhaled or swallowed.
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