|
|
| General |
| Name, Symbol,
Number |
thorium, Th, 90 |
| Chemical series |
Actinides |
| Group, Period,
Block |
n/a, 7,
f |
| Appearance |
silvery white |
| Standard atomic weight |
232.03806(2)
g·mol−1 |
| Electron configuration |
[Rn] 6d2 7s2 |
| Electrons per shell |
2, 8, 18, 32, 18, 10, 2 |
| Physical properties |
| Phase |
solid |
| Density (near r.t.) |
11.7 g·cm−3 |
| Melting point |
2115 K
(1842 °C, 3348 °F) |
| Boiling point |
5061 K
(4788 °C, 8650 °F) |
| Heat of fusion |
13.81 kJ·mol−1 |
| Heat of vaporization |
514 kJ·mol−1 |
| Heat capacity |
(25 °C) 26.230 J·mol−1·K−1 |
Vapor pressure
| P(Pa) |
1 |
10 |
100 |
1 k |
10 k |
100 k |
| at T(K) |
2633 |
2907 |
3248 |
3683 |
4259 |
5055 |
|
| Atomic properties |
| Crystal structure |
cubic face centered |
| Oxidation states |
4
(weakly basic oxide) |
| Electronegativity |
1.3 (scale Pauling) |
Ionization energies
(more) |
1st: 587 kJ·mol−1 |
| 2nd: 1110 kJ·mol−1 |
| 3rd: 1930 kJ·mol−1 |
| Atomic radius |
180 pm |
| Miscellaneous |
| Magnetic ordering |
no data |
| Electrical resistivity |
(0 °C) 147 nΩ·m |
| Thermal conductivity |
(300 K) 54.0 W·m−1·K−1 |
| Thermal expansion |
(25 °C) 11.0 µm·m−1·K−1 |
| Speed of sound (thin rod) |
(20 °C) 2490 m/s |
| Young's modulus |
79 GPa |
| Shear modulus |
31 GPa |
| Bulk modulus |
54 GPa |
| Poisson ratio |
0.27 |
| Mohs hardness |
3.0 |
| Vickers hardness |
350 MPa |
| Brinell hardness |
400 MPa |
| CAS registry number |
7440-29-1 |
| Selected isotopes |
|
|
| References |
Thorium (IPA: /ˈθɔːriəm/) is a chemical element in the periodic table that has the symbol Th and atomic number 90.
As a naturally occurring, slightly radioactive metal, it has been considered as an alternative nuclear fuel to uranium.
Notable characteristics
When pure, thorium is a silvery white metal that retains its luster for several months. However, when it is exposed to oxygen,
thorium slowly tarnishes in air, becoming grey and eventually black. Thorium dioxide
(ThO2), also called thoria, has the highest melting point of any oxide (3300°C)[1]. When heated in air, thorium metal turnings ignite
and burn brilliantly with a white light.
Thorium has the largest liquid range of any element: 2946°C (2946 K) between the melting point and boiling point.
See Actinides in the environment for details of the environmental
aspects of thorium.
Applications
Applications of thorium:
Applications of thorium dioxide (ThO2):
- Mantles in portable gas lights. These mantles glow with a dazzling light (unrelated to
radioactivity) when heated in a gas flame.
- Used to control the grain size of tungsten used for electric lamps.
- Used for high-temperature laboratory crucibles.
- Added to glass, it helps create glasses of a high refractive index and with low dispersion. Consequently,
they find application in high-quality lenses for cameras and scientific instruments.
- Has been used as a catalyst:
- Thorium dioxide is the active ingredient of Thorotrast, which was used as part of
X-ray diagnostics. This use has been abandoned due to the carcinogenic nature of Thorotrast.
History
M. T. Esmark found a black mineral on Løvøy Island, Norway and gave a sample to Professor
Jens Esmark, a noted mineralogist who was not able to
identify it so he sent a sample to the Swedish chemist Jöns Jakob Berzelius for
examination in 1828.[2] Berzelius analysed it and named it
after Thor, the Norse god of thunder. The metal had
virtually no uses until the invention of the gas mantle in 1885.
The crystal bar process (or Iodide process) was discovered by
Anton Eduard van Arkel and Jan Hendrik de Boer in
1925 to produce high-purity metallic thorium. [3]
The name ionium was given early in the study of radioactive elements to the 230Th isotope produced in the decay chain of 238U before it was realized that ionium and thorium were chemically identical. The symbol
Io was used for this supposed element.
Occurrence
Monazite, a rare-earth-and-thorium-phosphate mineral, is the primary source of the world's thorium
Thorium is found in small amounts in most rocks and soils, where it is about three times more
abundant than uranium, and is about as common as lead. Soil
commonly contains an average of around 12 parts per million (ppm) of thorium. Thorium occurs in several minerals, the most common being the rare earth-thorium-phosphate mineral, monazite, which contains up to about 12% thorium oxide. There are substantial deposits in several countries.
232Th decays very slowly (its half-life is about three times the age of the earth)
but other thorium isotopes occur in the thorium and uranium decay chains. Most of these are short-lived and hence much more radioactive than 232Th,
though on a mass basis they are negligible. India is believed to have 25% of the world's Thorium reserves. [4]
See also thorium minerals.
Distribution
Present knowledge of the distribution of Thorium resources is poor because of the relatively low-key exploration efforts
arising out of insignificant demand.[5] Under the
prevailing estimate, Australia and India have particularly
large reserves of thorium.
- The prevailing estimate of the economically available thorium reserves comes from the US Geological Survey, Mineral Commodity
Summaries (1997-2006):[6][7]
| Country |
Th Reserves (tonnes) |
Th Reserve Base (tonnes) |
| Australia |
300,000 |
340,000 |
| India |
290,000 |
300,000 |
| Norway |
170,000 |
180,000 |
| United States |
160,000 |
300,000 |
| Canada |
100,000 |
100,000 |
| South Africa |
35,000 |
39,000 |
| Brazil |
16,000 |
18,000 |
| Malaysia |
4,500 |
4,500 |
| Other Countries |
95,000 |
100,000 |
| World Total |
1,200,000 |
1,400,000 |
- Another estimate of Reasonably Assured Reserves (RAR) and Estimated Additional Reserves (EAR) of thorium comes from OECD/NEA,
Nuclear Energy, "Trends in Nuclear Fuel Cycle", Paris, France (2001)[8]
| Country |
RAR Th (tonnes) |
EAR Th (tonnes) |
| Brazil |
606,000 |
700,000 |
| Turkey |
380,000 |
500,000 |
| India |
319,000 |
- |
| United States |
137,000 |
295,000 |
| Norway |
132,000 |
132,000 |
| Greenland |
54,000 |
32,000 |
| Canada |
45,000 |
128,000 |
| Australia |
19,000 |
- |
| South Africa |
18,000 |
- |
| Egypt |
15,000 |
309,000 |
| Other Countries |
505,000 |
- |
| World Total |
2,230,000 |
2,130,000 |
The two sources vary wildly for countries such as Brazil, Turkey, and Australia.
Thorium as a nuclear fuel
Thorium metal foil (approximately 0.5 mm thick) sealed in a glass ampoule under an argon atmosphere to prevent oxidation
Thorium, as well as uranium and plutonium, can be used as
fuel in a nuclear reactor. Although not fissile itself, 232Th will absorb slow neutrons to
produce uranium-233 (233U), which is fissile. Hence, like 238U, it is fertile. In one significant respect
233U is better than the other two fissile isotopes used for nuclear fuel, 235U and plutonium-239
(239Pu), because of its higher neutron yield per neutron absorbed. Given a start with some other fissile material
(235U or 239Pu), a breeding cycle similar to, but more efficient than that currently possible with the
238U-to-239Pu cycle (in slow-neutron reactors), can be set up. The
232Th absorbs a neutron to become 233Th which normally decays to protactinium-233 (233Pa) and then 233U. The irradiated fuel can then be unloaded from
the reactor, the 233U separated from the thorium (a relatively simple process since it involves chemical instead of
isotopic separation), and fed back into another reactor as part of a closed nuclear fuel
cycle.
Problems include the high cost of fuel fabrication due partly to the high radioactivity of 233U which is a result
of its contamination with traces of the short-lived 232U; the similar problems in recycling thorium due to highly
radioactive 228Th; some weapons proliferation risk of 233U; and the technical problems (not yet
satisfactorily solved) in reprocessing. Much development work is still required before the thorium fuel cycle can be
commercialised, and the effort required seems unlikely while (or where) abundant uranium is available.
Nevertheless, the thorium fuel cycle, with its potential for breeding fuel without
fast neutron reactors, holds considerable potential long-term benefits. Thorium is
significantly more abundant than uranium, and is a key factor in sustainable nuclear energy.
India, having about 25% of the world's reserves [4], has planned its nuclear power program to eventually use thorium exclusively,
phasing out uranium as a feed stock. This ambitious plan uses both fast and thermal breeder
reactors. The Advanced Heavy Water Reactor and KAMINI reactor are efforts in this direction.
In 2007, Norway was debating whether or not to focus on Thorium plants.
The primary fuel of the HT3R Project in Odessa, Texas,
USA will be Ceramic-coated thorium beads.
Isotopes
-
Naturally occurring thorium is composed of one isotope: 232Th. Twenty-seven radioisotopes have been characterized,
with the most abundant and/or stable being 232Th with a half-life of 14.05 billion
years, 230Th with a half-life of 75,380 years, 229Th with a half-life of 7340 years, and 228Th
with a half-life of 1.92 years. All of the remaining radioactive isotopes have half-lives
that are less than thirty days and the majority of these have half-lives that are less than ten minutes. One isotope,
229Th, has a nuclear isomer (or metastable state) with a remarkably low
excitation energy of 3.5 eV. [9]
The known isotopes of thorium range in atomic weight from 210 u (210Th)[10] to 236 u
(236Th).
Precautions
Powdered thorium metal is often pyrophoric and should be handled carefully.
Natural thorium decays very slowly compared to many other radioactive materials, and the alpha
radiation emitted cannot penetrate human skin. Owning and handling small amounts of thorium, such as a gas mantle, is considered safe if care is taken not to ingest the thorium -- lungs and other internal organs
can be penetrated by alpha radiation. Exposure to aerosolized thorium can lead to increased risk of cancers of the lung, pancreas and
blood. Exposure to thorium internally leads to increased risk of liver diseases. This element has no known biological role. See also Thorotrast.
Thorium Extraction
Thorium has been extracted chiefly from monazite through a multi-stage process. In the first stage, the monazite sand is
dissolved in an inorganic acid such as sulfuric acid (H2SO4). In the second, the Thorium is extracted into
an organic phase containing an amine. Next it is separated or "stripped" using an anion such as nitrate, chloride, hydroxide, or
carbonate, returning the thorium to an aqueous phase. Finally, the thorium is precipitated and collected.[11]
See also
References
- ^ Emsley, John (2001).
Nature's Building Blocks, (Hardcover, First Edition), Oxford University
Press, page 441. ISBN 0198503407.
- ^ Thorium. BBC.co. Retrieved on 2007-01-18.
- ^ van Arkel, A.E.; de Boer, J.H. (1925).
"Preparation of pure titanium, zirconium, hafnium, and thorium metal". Zeitschrift für Anorganische und Allgemeine Chemie
148: 345-350. Retrieved on 2006-05-06.
- ^ a b US approves Indian nuclear deal. BBC News (2006-12-09).
- ^ K.M.V. Jayaram. An Overview of World Thorium
Resources, Incentives for Further Exploration and Forecast for Thorium Requirements in the Near Future.
- ^ U.S. Geological
Survey, Mineral Commodity Summaries - Thorium.
- ^ Information and Issue Briefs - Thorium. World Nuclear Association. Retrieved on 2006-11-01.
- ^ IAEA: Thorium fuel cycle --
Potential benefits and challenges, pp 45(table 8), 97(ref 78).
- ^ Phys. Rev. C 73 044326 (April 2006)
- ^ Phys. Rev. C 52, 113–116 (1995)
- ^ Crouse, David; Brown, Keith (December 1959). "The Amex Process for Extracting Thorium Ores with Alkyl Amines".Industrial & Engineering Chemistry
51 (12): 1461. Retrieved on 2007-03-09
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