Thorium

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What is Thorium?

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Thorium (chemical symbol Th, atomic number 90) is a naturally occurring, weakly radioactive metallic element. It was discovered in 1828 by Swedish chemist Jöns Jakob Berzelius, who named it after Thor, the Norse god of thunder. Thorium is a member of the actinide series on the periodic table.

In nature, thorium exists almost entirely as Thorium-232 (Th-232), with a half-life of approximately 14.05 billion years — roughly three times the age of the Earth. This extreme stability means thorium ore poses very little immediate radiation hazard during mining or handling.

Abundance and Distribution

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Thorium is approximately 3 to 4 times more abundant than uranium in the Earth's crust, with an average crustal concentration of around 6–10 parts per million. It is found in many common minerals, most notably:

  • Monazite — a phosphate mineral that is the primary commercial source of thorium, also rich in rare earth elements
  • Thorite (ThSiO₄)
  • Thorianite (ThO₂)
  • Bastnäsite

Monazite sand deposits — heavy mineral sands found on beaches and in riverbeds — are especially rich sources and are found in Australia, India, Brazil, the United States, South Africa, Canada, and throughout Southeast Asia.

World Thorium Reserves (Estimated)

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Country Estimated Reserves (tonnes)
India 846,000
Brazil 632,000
Australia 595,000
United States 440,000
Egypt 380,000
Norway 132,000
Turkey 344,000
Venezuela 300,000
Canada 172,000
South Africa 148,000
Other countries ~750,000
World Total ~6,355,000+

Note: China's thorium reserves are not included in most public IAEA estimates, but are believed to be substantial.

Physical and Chemical Properties

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  • Atomic weight: 232.038
  • Melting point: 1,750 °C (3,182 °F)
  • Boiling point: 4,788 °C (8,650 °F)
  • Density: 11.7 g/cm³
  • Appearance: Silvery-white metal, tarnishes to grey or black on exposure to air
  • Radioactive decay: Alpha emitter; decays very slowly through a long chain eventually to lead-208

Thorium as Nuclear Fuel

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Thorium-232 is fertile but not fissile. It cannot undergo sustained nuclear fission by thermal neutrons without first being converted into fissile U-233. This conversion is achieved by neutron capture and subsequent radioactive decay (see: Thorium Fuel Cycle).

One tonne of thorium, if fully converted and fissioned in a well-designed reactor, can yield energy equivalent to approximately:

  • 200 tonnes of uranium oxide (for use in a conventional LWR)
  • 3.5 million tonnes of coal

The global identified thorium resource of over 6 million tonnes therefore represents an essentially inexhaustible energy supply if used in breeder reactors — sufficient to power human civilisation for thousands of years at current consumption levels.

Non-Energy Uses

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Before its nuclear potential was recognised, thorium was used commercially in:

  • Gas mantles: Thorium oxide was used in incandescent gas mantles throughout the late 19th and early 20th centuries.
  • Refractory materials: Thorium oxide (ThO₂) has an extremely high melting point (3,300 °C) and was used in high-temperature crucibles and heating elements.
  • Alloys: Small quantities of thorium improve the high-temperature strength of magnesium and other alloys.
  • Optics: Thoriated lenses (camera and telescope glass) were produced until the 1970s. Photographers still use vintage thoriated lenses today.
  • Welding electrodes: Thoriated tungsten electrodes (2% ThO₂) produce a more stable arc and are still used in TIG welding, though alternatives are increasingly being adopted due to radioactivity concerns.

See Also

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