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Thorium (Th)
Thorium (Th) is a radioactive chemical element with the atomic number 90, belonging to the actinide series of the periodic table. It resembles uranium in its chemical and physical properties and is primarily found in minerals such as monazite, which is commonly located in sand deposits across various countries including India, Brazil, Australia, and parts of the United States. The most significant isotope of thorium is thorium-232, which has a notably long half-life of about fourteen billion years and can be converted into uranium-233 for use in nuclear reactors.
Historically, thorium was discovered in 1828 and initially used in incandescent gaslight mantles due to its ability to emit bright light when heated. Today, it has various applications beyond nuclear energy, including strengthening magnesium alloys, making photoelectric cells, and serving as a catalyst in different chemical processes. However, thorium's radioactivity poses health risks, particularly from its decay product radon-220, which can be harmful if inhaled. As a result, the use of thorium-based products has diminished in recent years.
Authored By: Secrest, Rose 1 of 4
Published In: 2020 2 of 4
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Where Found
Thorium occurs in various minerals that contain uranium or rare earth elements. The most important source of thorium is monazite, which is usually found in sand. Sand containing monazite is found in India, Brazil, Australia, Madagascar, Sri Lanka, South Africa, and Canada. In the United States, thorium is found in Idaho, Florida, Michigan, California, Colorado, North Carolina, and South Carolina.
Primary Uses
Thorium is mostly used in the form of thorium 232. This can be used to produce uranium 233 for nuclear reactors.
Technical Definition
Thorium (abbreviated Th), atomic number 90, belongs to the actinide series of the periodic table of the elements and resembles uranium in its chemical and physical properties. All thorium isotopes are radioactive; thorium 232 dominates because it has a half-life of about fourteen billion years. Thorium has an atomic weight of 232.038. Pure thorium is a silver-white metal that turns gray or black when exposed to air. Its density is 11.7 grams per cubic centimeter; it has a melting point of about 1,700° Celsius and a boiling point of about 4,000° Celsius. (Exact figures cannot be given because these values are greatly changed by impurities.)
Description, Distribution, and Forms
Thorium is a fairly rare radioactive element resembling uranium. It is mostly obtained along with rare earth elements in the processing of monazite. Thorium serves as an indirect source of nuclear power because it can be changed into uranium.
History
Thorium was discovered in 1828 by the Swedish chemist Jöns Jacob Berzelius. Its radioactive nature was discovered in 1898. In the late nineteenth century and early twentieth century, thorium was mostly used in mantles for incandescent gaslights because it gave off a bright white light when heated.
Obtaining Thorium
Thorium is usually obtained from monazite. First the monazite is finely ground and mixed with hot sulfuric acid or hot sodium hydroxide to separate thorium and rare earth elements from the other substances found in monazite. Thorium compounds are then obtained from this mixture by a variety of chemical reactions. In general, these methods depend on the fact that certain thorium compounds have different solubilities from similar compounds of the rare earth elements in certain solvents.
Free thorium may be obtained by treating thorium oxide with calcium at about 950° Celsius. It may also be obtained by the electrolysis of thorium chloride. The thorium powder obtained by these methods may be transformed into thorium metal by compressing it and heating it in a vacuum.
Uses of Thorium
In a nuclear reactor thorium 232 can be transformed into uranium 233, which can undergo fission to release nuclear energy. Thorium is also used to strengthen magnesium alloys, to make photoelectric cells, as a catalyst, in welding electrodes, and in high-temperature ceramics.
Because thorium is radioactive, it poses a health hazard. Although thorium 232 is not particularly dangerous on its own, one of the substances it changes into as it decays, radon 220, is hazardous because it is a gas and may enter the lungs. Because of its radioactivity, the use of thorium products has decreased.
Bibliography
U.S. Geological Survey.
Mineral Information: Thorium Statistics and Information. http://minerals.usgs.gov/minerals/pubs/commodity/thorium/
Full Article
Where Found
Thorium occurs in various minerals that contain uranium or rare earth elements. The most important source of thorium is monazite, which is usually found in sand. Sand containing monazite is found in India, Brazil, Australia, Madagascar, Sri Lanka, South Africa, and Canada. In the United States, thorium is found in Idaho, Florida, Michigan, California, Colorado, North Carolina, and South Carolina.
Primary Uses
Thorium is mostly used in the form of thorium 232. This can be used to produce uranium 233 for nuclear reactors.
Technical Definition
Thorium (abbreviated Th), atomic number 90, belongs to the actinide series of the periodic table of the elements and resembles uranium in its chemical and physical properties. All thorium isotopes are radioactive; thorium 232 dominates because it has a half-life of about fourteen billion years. Thorium has an atomic weight of 232.038. Pure thorium is a silver-white metal that turns gray or black when exposed to air. Its density is 11.7 grams per cubic centimeter; it has a melting point of about 1,700° Celsius and a boiling point of about 4,000° Celsius. (Exact figures cannot be given because these values are greatly changed by impurities.)
Description, Distribution, and Forms
Thorium is a fairly rare radioactive element resembling uranium. It is mostly obtained along with rare earth elements in the processing of monazite. Thorium serves as an indirect source of nuclear power because it can be changed into uranium.
History
Thorium was discovered in 1828 by the Swedish chemist Jöns Jacob Berzelius. Its radioactive nature was discovered in 1898. In the late nineteenth century and early twentieth century, thorium was mostly used in mantles for incandescent gaslights because it gave off a bright white light when heated.
Obtaining Thorium
Thorium is usually obtained from monazite. First the monazite is finely ground and mixed with hot sulfuric acid or hot sodium hydroxide to separate thorium and rare earth elements from the other substances found in monazite. Thorium compounds are then obtained from this mixture by a variety of chemical reactions. In general, these methods depend on the fact that certain thorium compounds have different solubilities from similar compounds of the rare earth elements in certain solvents.
Free thorium may be obtained by treating thorium oxide with calcium at about 950° Celsius. It may also be obtained by the electrolysis of thorium chloride. The thorium powder obtained by these methods may be transformed into thorium metal by compressing it and heating it in a vacuum.
Uses of Thorium
In a nuclear reactor thorium 232 can be transformed into uranium 233, which can undergo fission to release nuclear energy. Thorium is also used to strengthen magnesium alloys, to make photoelectric cells, as a catalyst, in welding electrodes, and in high-temperature ceramics.
Because thorium is radioactive, it poses a health hazard. Although thorium 232 is not particularly dangerous on its own, one of the substances it changes into as it decays, radon 220, is hazardous because it is a gas and may enter the lungs. Because of its radioactivity, the use of thorium products has decreased.
Bibliography
U.S. Geological Survey.
Mineral Information: Thorium Statistics and Information. http://minerals.usgs.gov/minerals/pubs/commodity/thorium/
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