Thorium is a silvery, slightly radioactive actinide metal. It is mainly found as ThO₂ (thoria) in monazite sands and is used in high-temperature ceramics, gas mantles historically, and as a fertile material (Th-232 → U-233) in some nuclear fuel cycles.
Thorium (Th) is an actinide metal with atomic number 90. It sits in period 7 and belongs to the f-block, immediately after actinium and before protactinium.
Natural thorium is predominantly \(^{232}\mathrm{Th}\), which has an extremely long half-life (on the order of \(10^{10}\) years). Because it decays very slowly, the specific activity (radioactivity per gram) is relatively low compared to short-lived radionuclides, hence it is described as slightly radioactive.
Thorium itself is fertile (not fissile). In a neutron field, it captures a neutron and undergoes two beta decays to become fissile uranium-233:
The produced \(^{233}\mathrm{U}\) can then sustain a nuclear chain reaction.
Thorium most commonly forms the +4 oxidation state (\(\mathrm{Th^{4+}}\)), though lower states like +3 are known in special contexts. A ground-state configuration is often given as [Rn] 6d2 7s2 (with f-electron participation context-dependent in bonding for actinides).
Thorium occurs mainly as thoria (\(\mathrm{ThO_2}\)) in monazite sands, a phosphate mineral rich in rare-earth elements. Processing typically involves:
Thoria has a very high melting point (\(> 3000^{\circ}\mathrm{C}\)), excellent refractoriness, and good ionic conductivity at high temperature. Historically, it was used in gas mantles, and today it finds use in specialized high-temperature ceramics and research applications.
Although only slightly radioactive, thorium is still a radiotoxic heavy metal. Good practice includes:
Key compounds include thorium(IV) oxide \(\mathrm{ThO_2}\), thorium(IV) chloride \(\mathrm{ThCl_4}\), and thorium(IV) nitrate \(\mathrm{Th(NO_3)_4}\). Thorium(IV) tends to form hydrolyzed and polymeric species in aqueous solution; \(\mathrm{ThO_2}\) is notably insoluble and chemically robust.
Yes. \(^{232}\mathrm{Th}\) is the head of the thorium decay series, which proceeds via a chain of \(\alpha\)- and \(\beta\)-decays through nuclides such as radium, radon, and polonium, eventually ending at stable \(^{208}\mathrm{Pb}\).