Chemical Fact Sheet
Uranium
| Chemical Abstract Number (CAS #) | 7440-61-1 |
|---|---|
| Synonyms | URANIUM-I- ((238)U) |
| Analytical Methods | 200.8 - 6020 |
| Molecular Formula | U |
|
Synopsis |
Uranium-(Planet Uranus), U; at. wt. 238.0289(1); at.
no. 92; m.p. 1135 deg C; b.p. 4131 deg C; sp. gr. ~18.95; valence 2, 3,
4, 5, or 6. Yellow-colored glass, containing more than 1% uranium oxide
and dating back to 79 A.D., has been found near Naples, Italy. Klaproth
recognized an unknown element in pitchblende and attempted to isolate the
metal in 1789. The metal apparently was first isolated in 1841 by Peligot,
who reduced the anhydrous chloride with potassium. Uranium is not as rare
as it was once thought. It is now considered to be more plentiful than
mercury, antimony, silver, or cadmium, and is about as abundant as molybdenum
or arsenic. It occurs in numerous minerals such as pitchblende, uraninite,
carnotite, autunite, uranophane, davidite, and tobernite. It is also found
in phosphate rock, lignite, monazite sands, and can be recovered commercially
from these sources. Large deposits of uranium ore occur in Utah, Colorado,
New Mexico, Canada, and elsewhere. The U.S.D.O.E. purchases uranium in
the form of acceptable U3O8 concentrates. This incentive program has greatly
increased the known uranium reserves. Uranium can be made by reducing uranium
halides with alkali or alkaline earth metals or by reducing uranium oxides
by calcium, aluminum, or carbon at high temperatures. The metal can also
be produced by electrolysis of KUF5 or UF4, dissolved in a molten mixture
of CaCl2 and NaCl. High-purity uranium can be prepared by the thermal decomposition
of uranium halides on a hot filament. Uranium exhibits three crystallographic
modifications as follows:
alpha---688 deg C--->beta---776 deg C--->gamma Uranium is a heavy, silvery-white metal which is pyrophoric when finely divided. It is a little softer than steel, and is attacked by cold water in a finely divided state. It is malleable, ductile, and slightly paramagnetic. In air, the metal becomes coated with a layer of oxide. Acids dissolve the metal, but it is unaffected by alkalis. Uranium has twenty three isotopes, one of which is an isomer and all of which are radioactive. Naturally occurring uranium contains 99.2745% by weight 238U, 0.720% 235U, and 0.0055% 234U. Studies show that the percentage weight of 235U in natural uranium varies by as much as 0.1% depending on the source. The U.S.D.O.E. has adopted the value of 0.711 as being their "official" percentage of 235U in natural uranium. Natural uranium is sufficiently radioactive to expose a photographic plate in an hour or so. Much of the internal heat of the earth is thought to be attributable to the presence of uranium and thorium. 238U with a half-life of 4.46 x 10^9 years, has been used to estimate the age of igneous rocks. The origin of uranium, the highest member of the naturally occurring elements - except perhaps for traces of neptunium or plutonium - is not clearly understood, although it may be presumed that uranium is a decay product of elements of higher atomic weight, which may have once been present on earth or elsewhere in the universe. These original elements may have been formed as a result of a primordial "creation," known. as "the big bang," in a supenova, or in some other stellar processes. Uranium is of great importance as a nuclear fuel. 238U can be converted into fissionable plutonium by the following reactions: 238U(n,y)-->239U--B-->239Np--B-->239Pu This nuclear conversion can be brought about in "breeder" reactors where it is possible to produce more new fissionable material than the fissionable material used in maintaining the chain reaction. 235U is of even greater importance, for it is the key to the utilization of uranium. 235U, while occurring in natural uranium to the extent of only 0.71 %, is so fissionable with slow neutrons that a self-sustaining fission chain reaction can be made to occur in a reactor constructed from natural uranium and a suitable moderator, such as heavy water or graphite, alone. 235U can be concentrated by gaseous diffusion and other physical processes, if desired, and used directly as a nuclear fuel, instead of natural uranium, or used as an explosive. Natural uranium, slightly enriched with 235U by a small percentage, is used to fuel nuclear power reactors for the generation of electricity. Natural thorium can be irradiated with neutrons as follows to produce the important isotope 233U. 232Th(n,y)-->233Th--B-->233Pa--B-->233U While thorium itself is not fissionable, 233U is, and in this way may be used as a nuclear fuel. One pound of completely fissioned uranium has the fuel value of over 1500 tons of coal. The uses of nuclear fuels to generate electrical power, to make isotopes for peaceful purposes, and to make explosives are well known. The estimated world-wide production of the 430 nuclear power reactors in operation in January 1994 amounted to about 338,000 megawatts. Uranium in the U.S.A. is controlled by the U.S. Nuclear Regulatory Commission. New uses are being found for "depleted" uranium, i.e., uranium with the percentage of 235U lowered to about 0.2%. It has found use in inertial guidance devices, gyro compasses, counterweights for aircraft control surfaces, as ballast for missile reentry vehicles, and as a shielding material. Uranium metal is used for X-ray targets for production of high-energy X-rays; the nitrate has been used as photographic toner, and the acetate is used in analytical chemistry. Crystals of uranium nitrate are triboluminescent. Uranium salts have also been used for producing yellow "vaseline" glass and glazes. Uranium and its compounds are highly toxic, both from a chemical and radiological standpoint. Finely divided uranium metal, being pyrophoric, presents a fire hazard. The maximum permissible total body burden of natural uranium (based on radiotoxicity) is 0.2 uCi for soluble compounds. Recently, the natural presence of uranium in many soils has become of concern to homeowners because of the generation of radon and its daughters (see under Radon). Uranium metal is available commercially at a cost of about $200/kg (99.7%) in air-tight glass under argon. |
| Apparent Color | SILVER-WHITE, LUSTROUS, METAL; A BLACK POWDER WHEN OBTAINED BY REDUCTION; THREE ALLOTROPHIC MODIFICATIONS: ORTHORHOMBIC ALPHA-FORM TO 667.7 DEG C; TETRAGONAL BETA-FORM FROM 667.7 DEG C TO 774.8 DEG C; BODY-CENTERED CUBIC, GAMMA-FORM FROM 774.8 DEG C TO MP |
| Boiling Point | 3818 DEG C |
| Melting Point | 1132.3 + or - 0.8 DEG C |
| Molecular Weight | 238.03 |
| Density | 19.05 + or - 0.02 @ 25 DEG C |
|
Chemical and Physical Properties |
METAL NOT AS HARD AS STEEL; DUCTILE, MALLEABLE, CAN BE MELTED & EXTRUDED AT HIGH TEMP; TAKES HIGH POLISH AFTER COLD WORKING. STRONGLY ELECTROPOSITIVE; POOR CONDUCTOR OF ELECTRICITY; HEAT CAPACITY 6.6 CAL/MOL/DEG C; DENSE SOLID; FORMS SOLID SOLN WITH MOLYBDENUM, NIOBIUM, TITANIUM, ZIRCONIUM; METAL REACTS WITH NEARLY ALL NONMETALS; HEAT OF FUSION: 4.7 KCAL/MOLE ALPHA EMITTER, ONLY WEAKLY RADIOACTIVE 14 ISOTOPES ALL RADIOACTIVE Pure uranium metal is very reactive as a strong reducing agent. ATOMIC NUMBER 92; NOT ATTACKED BY ALKALIES; SPECIFIC HEAT 6.65 CAL/G ATOM/DEG C @ 25 DEG C; ON VIGOROUS SHAKING THE METALLIC PARTICLES EXHIBIT LUMINESCENCE; BURNS IN FLUORINE TO PRODUCE MAINLY A GREEN VOLATILE TETRAFLUORIDE; IN CHLORINE @ 180 DEG C, IN BROMINE @ 240 DEG C; FORMS AN IODIDE @ 260 DEG C; REACTS WITH ACIDS WITH LIBERATION OF HYDROGEN & FORMATION OF SALTS OF TETRAVALENT URANIUM; ATTACKED BY DRY HYDROGEN CHLORIDE AT A DULL RED HEAT WITH FORMATION OF A STABLE CHLORIDE; COMBINES WITH SULFUR @ 500 DEG C, WITH NITROGEN @ 1000 DEG C. Radiation from uranium has low penetration & elaborate shielding is unnecessary. |
|
Environmental Impact |
Natural uranium is present in soils & rocks in concn generally varying between 0.5 & 5 ppm. The avg is approx 1.8 ppm in most soils. URANIUM MINING HAS NOT BEEN ASSOCIATED WITH MEASURABLE INCREASES IN ENVIRONMENTAL RADIOACTIVITY OUTSIDE IMMEDIATE VICINITY OF MINES. FOR URANIUM MILLS & FUEL FABRICATION PLANTS PROPER LOCATION & APPROPRIATE CONTROL OF TAILINGS & LIQUID WASTES CAN PREVENT SIGNIFICANT POPULATION EXPOSURES. Inhalation, skin & eye contact, lung. The avg daily dietary intake of uranium by man is 1 to 1.5 ug. AN OCCUPATIONAL EXPOSURE PROBLEM OF SUBSTANTIAL MAGNITUDE INVOLVES MINERS WHO WORK UNDERGROUND IN URANIUM MINES. Hazards from the production of uranium metal briquettes or in the hot-rolling of uranium rods are relatively small. Exposures of majority of the uranium plant workers were to dust of uranium feed materials to the intermediates, to uranium metal. The isotope most dangerous from the point of view of radiation, (235)uranium, comprises less than 1% of natural uranium, but is enriched during the production of nuclear fuels. Higher fractions of (235)uranium increase the irradiation risk. The following list includes some common operations in which exposure to uranium or insol cmpd may occur liberation from mining, grinding, & milling of ores; use of insol cmpd as chemical intermediates in prepn of uranium cmpd; use for nuclear technology; use in nuclear reactors as fuel & to pack nuclear fuel rods; liberation from burning of uranium metal chips & smelting operations; use in ceramics industry for pigments, coloring porcelain, & enamelling; use as catalysts for many reactions; in production of fluorescent glass. OCCUPATIONAL EXPOSURE TO URANIUM USUALLY INVOLVES MIXTURES OF DIFFERENT URANIUM CMPD WITH SOLUBILITES IN WATER AT ROOM TEMP RANGING FROM 1 TO 400,000 MG U/L. DUST PARTICLES CONTAINING URANIUM MAY BE OF VARYING SIZES & DENSITIES. The uranium content of human tissues obtained at autopsy reviewed, and est were made of uranium in human bone and soft tissues. The range of natural uranium in the human skeleton (2-62 ug) is attributed to geographic variation and to analytical and sampling uncertainties. Uranium in the skeleton is believed to be roughly in equilibrium with intake. The natural uranium content of an adult human kidney is approx 0.1 ug or approx 0.004 ug/g kidney tissue. Careful measurements of uranium concn in human bones from Nepal and Australia were made. The researchers calculated the annual alpha doses to bone from (238)uranium to be 0.039 mrad for the Nepalese and 0.009 mrad for the Australians. Such wide variations are not unexpected because of the known geographic differences in uranium concn in human bone. UNDER STEADY-STATE CONDITIONS IN OCCUPATIONALLY EXPOSED SUBJECTS, 85% OF THE BODY BURDEN OF URANIUM WAS FOUND IN BONE PROVIDED THAT URANIUM DEPOSITED IN THE LUNG IS EXCLUDED. MORE THAN 90% OF THE REMAINING URANIUM WAS IN THE KIDNEY, & DETECTABLE AMT COULD BE FOUND IN LIVER. Human body burden: Uranium 0.02 mg/70 kg. |
|
Environmental Fate |
URANIUM IS WIDELY DISTRIBUTED IN NATURE & ACCOUNTS FOR 3 TO 4X10-4% OF EARTH CRUST 2X10-5%. IT IS PRESENT IN A VARIETY OF MINERALS & IS ALSO ENCOUNTERED IN SEA WATER. CHIEF NATURAL SOURCES ARE HYDROTHERMAL VEINS IN SAXONY, ZAIRE, & CANADA; SEDIMENTARY ROCKS IN COLORADO, UTAH & NEW MEXICO; & PYRITIC CONGLOMERATE BEDS OF PRECAMBRIAN AGE IN WITWATERSTRAND & ONTARIO. Uranium is an important constituent of about 155 minerals; in another 60 minerals, it is a minor constituent or an impurity. IT OCCURS IN NUMEROUS MINERALS SUCH AS URANITE AUTUNITE, URANOPHANE, DAVIDITE & TOBERNITE. IT IS ALSO FOUND IN PHOSPHATE ROCK, LIGNITE, & MONAZITE SANDS. Selected uranium minerals: Euxenite, polycrase, fergusonite, samarskite, pyrochlore, microlite, brannerite, tyuyamunite, coffinite, thucholite. PITCHBLENDE FOUND IN COLORADO, UTAH, BEAR LAKE IN CANADA, ZAIRE, JOACHIMSTAHL IN CZECHOSLOVAKIA, CORNWALL. Carnotite a mineral containing uranium occurs in Colorado, New Mexico, France, South Africa, Australia, USSR. Uranium content of: Igneous rocks, 0.008 wt%; and ore deposits, 0.1 - 0.9 wt%. Acidic rocks with a high silicate content, ie, granite, have a uranium content above average. ESTIMATED THAT THE AVERAGE URANIUM CONTENT OF THE TOP 30 CM OF SOIL IS 2.3 TONS/SQ KM. The uranium content of rocks varies widely but is generally higher than that in the earth's crust-on the avg 3 ug/g. Depleted uranium is a by product of the uranium enrichment process during which natural uranium is enriched by increasing the percentage of the (2350uranium isotope. Uranium has a complex radioactive decay scheme resulting in the emission of different radiations and the production of several radioactive daughter products. Uranium, thorium, radium, radon, lead, and polonium radionuclide concentrations in ground waters from the Hanford Site indicate that uranium, thorium, and radium are highly sorbed. Relative to radon, these radionuclides are low by factors of 1x10(-3) to 1x10(-6). Uranium sorption is likely due to its reduction from the hexavalent state, where it is introduced via surface waters, to the tetravalent state found in the confined aquifers. The distribution of radionuclides is very similar in all of the confined aquifiers and significantly different from the distribution observed in the unconfined and surface waters. Barium correlates well with radium over three orders of magnitude, indicating that stable element analogs may be useful for inferring the behavior of radioactive waste radionuclides in this candidate geologic repository. |
|
Disposal |
Disposal of wastes containing uranium should follow guidelines set forth by the Nuclear Regulatory Commission. |
|
Atmosphere |
Uranium concentrations in air up to several 100 ug/cu m have been reported for some occupational conditions. The United Nations (1977) estimated that the daily adult intake via inhalation is approx 1x10-3 picoCi. The United Nations (1971) estimated daily adult intake via inhalation is approx 1x10-5 pCi. |
| Alphabetical List of Compounds | |
| List of Compounds by CAS Number | |
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