Chalcogenidotetrelates are chemical compounds containing a group 14 element, known as a tetrel, and a group 16 element, known as a chalcogen. The group 14 elements are carbon, silicon, germanium, tin, lead and flerovium. Flerovium compounds like this are unknown due to its short half-life. The group 16 elements are oxygen, sulfur, selenium, tellurium, polonium and livermorium. Livermorium compounds like this are unknown due to its short half-life. Chalcogenidotetrelates are a class of chalcogenidometalates. In chalcogenidotetrelates, the chalcogen atom is normally divalent, and the tetrel atom is normally tetravalent. The chalcogen atom has one or two single bonds, or one double bond to tetrel atoms. The tetrel atom has one, two, three or four single bonds to chalcogen atoms, or one double bond plus one or two single bonds to chalcogen atoms. The tetrel atom would normally have four bonds in a +4 oxidation state. Carbon differs significantly from the other elements in seldom having four single bonds to chalcogens, and so has few compounds in this class such as orthocarbonates. [1]
Properties
Chalcogenidotetrelates form numerous structures, from zero-dimensional simple tetrahedra, clusters or supertetrahedra, one-dimensional chains, two-dimensional layers or three-dimensional networks, which may also be porous. [2]
Structures
The ortho-chalcogenidotetrelate anions [TE44− (T is a tetrel and E is a chalcogen) are tetrahedral in arrangement. A supertetrahedron can fuse 4 or 10 of these into a larger tetrahedral adamantane cluster [T4E104− eg [Ge4Se104−. [3] Dimers that share a corner have formula [T4E76−, and sharing an edge yield [T4E64−. [2]
Natural occurrence
Chalcogenidotetrelates encompass the most common minerals on Earth, and other terrestrial planets in the form of silicates and carbonates. Feldspar, olivine, pyroxene and calcite are common. Other chalcogenidotetrelate minerals containing sulfur and other elements are known.
Production
Chalcogenidotetrelates may be produced by heating together the chalcogen compounds of the desired ingredients. A high temperature flux of a molten salt may be used. Or solutions in amines or organic solvents may crystallise at low temperatures. [2]
Use
Chalcogenidotetrelates are researched to find ion-conductors, ion exchange materials, semiconductors, photovoltaics, photoluminescence, photocatalysts and non-linear optical materials. [2]
Related
Related materials include the chalcogenidotrielates, and organo-functionalized chalcogenidotetrelates, which have one or more organic groups attached to the tetrel atom. [2]
Subtypes
× Not known to exist.
Mixed chalcogen compounds or ions are also known. [2]
References
- ^ Dornsiepen, Eike; Geringer, Eugenie; Rinn, Niklas; Dehnen, Stefanie (February 2019). "Coordination chemistry of organometallic or inorganic binary group 14/16 units towards d-block and f-block metal atoms". Coordination Chemistry Reviews. 380: 136–169. doi: 10.1016/j.ccr.2018.09.001. S2CID 105580447.
- ^ a b c d e f Heine, Johanna; Dehnen, Stefanie (December 2012). "From Simple Chalcogenidotetrelate Precursors to Complex Structures and Functional Compounds". Zeitschrift für anorganische und allgemeine Chemie. 638 (15): 2425–2440. doi: 10.1002/zaac.201200319.
- ^ "Non-Classical Chalcogenido Metalates". Philipps-Universität Marburg. Retrieved 2021-07-17.
Further reading
- Laitinen, Risto; Oilunkaniemi, Raija (1 April 2019). Selenium and Tellurium Reagents: In Chemistry and Materials Science. Walter de Gruyter GmbH & Co KG. pp. 357–381. ISBN 978-3-11-052934-0.