# Pyrosilicate

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{{Chembox
| Verifiedfields = changed
| Watchedfields = changed
| verifiedrevid = 
| Name = Pyrosilicate anion
| IUPACName = Pyrosilicate
| OtherNames = disilicate, diorthosilicate
| ImageFile = Silicate-double-tetrahedra-3D-balls.png
| ImageClass = bg-transparent
| ImageSize = 200px
| ImageName = 
|Section1={{Chembox Identifiers
| InChI1 = 
| InChIKey1 = 
| CASNo_Ref = {{cascite|changed|CAS}}
| CASNo = 
| PubChem = 6857674
| ChemSpiderID = 5257009
| ChemSpiderID_Ref = {{chemspidercite|correct|chemspider}}
| ChEBI_Ref = {{ebicite|correct|EBI}}
| ChEBI = 29380
| Gmelin = 326578
| StdInChI_Ref = {{stdinchicite|correct|chemspider}}
| StdInChI = 1S/O7Si2/c1-8(2,3)7-9(4,5)6/q-6
| StdInChIKey_Ref = {{stdinchicite|correct|chemspider}}
| StdInChIKey = KUDCBYUNCUYIDU-UHFFFAOYSA-N
| SMILES = [O-][Si]([O-])([O-])O[Si]([O-])([O-])[O-]
}}
|Section2={{Chembox Properties
| MeltingPtC = 
| Formula_Charge = −6
| O=7 | Si=2 
| ConjugateAcid = [Pyrosilicic acid](/source/Pyrosilicic_acid)
}}
|Section3=
}}

A '''pyrosilicate''' is a type of [chemical compound](/source/chemical_compound); either an [ionic compound](/source/ionic_compound) that contains the '''pyrosilicate anion''' {{chem|Si|2|O|7|6-}}, or an [organic compound](/source/organic_compound) with the [hexavalent](/source/Valence_(chemistry))  ≡{{chem|O|3|Si}}-O-{{chem|Si|O|3}}≡ [group](/source/Moiety_(chemistry)). The anion is also called '''disilicate'''<ref name=chemspider>[http://www.chemspider.com/Chemical-Structure.5257009.html "Disilicate"]. ''Chemspider'' website, CSID:5257009,  Accessed 2018-05-26</ref> or '''diorthosilicate'''.

Ionic pyrosilicates can be considered [salts](/source/salt_(chemistry)) of the unstable [pyrosilicic acid](/source/pyrosilicic_acid), {{chem|H|6|Si|2|O|7}}.  Unlike the acid, the salts can be stable.  Indeed, pyrosilicates occur widely in nature as a class of [silicate minerals](/source/silicate_minerals), specifically the [sorosilicate](/source/sorosilicate)s - though some sorosilicate minerals, such as [gehlenite](/source/gehlenite), replace one of the silicon atoms with tetracoordinated [aluminium](/source/aluminium) or [boron](/source/boron), giving the [isostructural](/source/isostructural) anions {{chem2|AlSiO7(7-)}} and {{chem2|BSiO7(7-)}}.

Some notable synthetic pyrosilicates include
* [sodium pyrosilicate](/source/sodium_pyrosilicate) {{chem|Na|6|Si|2|O|7}}, a possible component of [water glass](/source/sodium_silicate).
* [sodium iron(II) pyrosilicate](/source/sodium_iron(II)_pyrosilicate) {{chem|Na|2|Fe|2|Si|2|O|7}}, a potential [cathode](/source/cathode) material for [batteries](/source/Battery_(electricity)).<ref name=pani>Abhishek Panigrahi, Shin-ichi Nishimura, Tatau Shimada, Eriko Watanabe, Wenwen Zhao, Gosuke Oyama, and Atsuo Yamada (2017): "Sodium Iron(II) Pyrosilicate {{chem|Na|2|Fe|2|Si|2|O|7}}: A Potential Cathode Material in the {{chem|Na|2|O}}-{{chem|FeO}}-{{chem|Si|O|2}} System". ''Chemistry of Materials'', volume 29, issue 10, pages 4361–4366. {{doi|10.1021/acs.chemmater.7b00764}}</ref>
* [sodium manganese(II) pyrosilicate](/source/sodium_manganese(II)_pyrosilicate) {{chem|Na|2|Mn|2|Si|2|O|7}}, another potential [cathode](/source/cathode) material.<ref name="renman1">Viktor Renman, Mario Valvo, 
Cheuk-Wai Tai, and Cesar Pay Gómez (2017): "Manganese Pyrosilicates as Novel Positive Electrode Materials for Na-Ion Batteries". Uppsala University Publications, DIVA [http://uu.diva-portal.org/smash/record.jsf?pid=diva2%3A1158595&dswid=4799 urn:nbn:se:uu:diva-334063]</ref><ref name="renman2">Viktor Renman (2017): "Structural and Electrochemical Relations in Electrode Materials for Rechargeable Batteries", Doctoral Thesis, Uppsala University, Department of Chemistry. ORCID: 0000-0001-8739-4054</ref>

==Structure==
The pyrosilicate anion can be described as two {{chem|Si|O|4}} [tetrahedra](/source/tetrahedron) that share a vertex (an [oxygen](/source/oxygen) atom).  The vertices that are not shared carry a negative charge each.

The structure of solid sodium pyrosilicate was described by [Volker Kahlenberg](/source/Volker_Kahlenberg) and others in 2010.<ref name=kahle>Volker Kahlenberg, Thomas Langreiter, and Erik Arroyabe (2010): "{{chem|Na|6|Si|2|O|7}} – The Missing Structural Link among Alkali Pyrosilicates". ''Zeitschrift für anorganishe und allgemeine Chemie'' (''Journal for Inorganic and General Chemistry''), volume  636, issue 11, pages 1974-1979. {{doi|10.1002/zaac.201000120}}</ref>

[Yuri Smolin](/source/Yuri_Smolin) and [Yuri Shepelev](/source/Yuri_Shepelev) determined in 1970 the crystal structures of pyrosilicates of [rare earth element](/source/rare_earth_element)s with generic formula {{chem|Ln|2|Si|2|O|7}}, where "Ln" stands for either one of [lanthanum](/source/lanthanum), [cerium](/source/cerium), [neodymium](/source/neodymium), [samarium](/source/samarium), [europium](/source/europium), [gadolinium](/source/gadolinium), [dysprosium](/source/dysprosium), [holmium](/source/holmium), [yttrium](/source/yttrium), [erbium](/source/erbium), [thulium](/source/thulium), or [ytterbium](/source/ytterbium).  They were found to belong to four distinct [crystallographic](/source/crystallography) classes, determined by the size of the [cation](/source/cation).<ref name=smolin>Yu. I. Smolin and Yu. F. Shepelev (1970): "The crystal structures of the rare earth pyrosilicates". ''Acta Crystallographica Section B'', volume B26, pages 484-492. {{doi|10.1107/S0567740870002698}}</ref>  Other researchers also studied [yttrium pyrosilicate](/source/yttrium_pyrosilicate) {{chem|Y|2|Si|2|O|7}}.,<ref name=anan/><ref name=dias >Dias, H.W.; Glasser, F.P.; Gunwardane, R.P.; and Howie, R.A. (1990): "The crystal structure of δ-yttrium pyrosilicate, δ-{{chem|Y|2|Si|2|O|7}}". ''Zeitschrift für Kristallographie'', volume 191, issues 1/2, pages 117-123; ISSN 0044-2968</ref> [gadolinium pyrosilicate](/source/gadolinium_pyrosilicate) {{chem|Gd|2|Si|2|O|7}}.,<ref name=dias/> and  [scandium pyrosilicate](/source/scandium_pyrosilicate) {{chem|Sc|2|Si|2|O|7}}.<ref name=anan>Anan'eva, G.V.; Karapetyan, V.E.; Korovkin, A.M.; Merkulyaeva, T.I.; Peschanskaya, I.A.; Savinova, I.P.; and Feofilov, P.P. (1982): "Strukturnye kharakteristiki i fizicheskie svojstva kristallov diorto(piro)silikatov lantanoidov, ittriya i skandiya, vyrashchennykh metodom Chokhral'skogo" ("Structural characteristics and physical properties of diortho(pyro)silicate crystals of lanthanides yttrium and scandium grown by the Czochralski technique"). ''Izv. Akad. Nauk SSSR, Neorg. Mater'' (translated in ''Inorganic Materials'', USA) volume 18, issue 3, pages 442-445. ISSN 0002-337X.</ref>

==Preparation==
Rare earth pyrosilicates {{chem|Ln|2|Si|2|O|7}} can be obtained by fusing the corresponding oxide {{chem|Ln|2|O|3}} with silica in 1:2 molar ratio,<ref name=smolin/>  Single crystals can be grown by the [Verneuil process](/source/Verneuil_process)<ref name=smolin/> or the [Czochralski method](/source/Czochralski_method).<ref name=anan/>

Industrial pyrosilicate can be produced by the depolymerisation of [metasilicate](/source/metasilicate) by alkali, which releases [water](/source/water) on breaking the {{chem2|Si\sO\sSi}} bond.<ref>{{cite patent|country=US|number=1953840|inventor=Myron C. Waddell|assign1=Grasselli Chemical Company|title=Process for making sodium pyrosilicate hydrate|status=patent|gdate=1934-04-03}}</ref> This proceeds according to the idealised equation
:{{chem2|2 SiO3(2-) + 2 OH(-) -> Si2O7(6-) + H2O}}
Additional alkali will degrade the bonds further, instead yielding [orthosilicate](/source/orthosilicate).<ref>{{cite patent|country=US|number=2351385A|status=patent|inventor=Eduard Zintl|gdate=1944-06-13|pridate=1939-11-11|title=Process of preparing anhydrous sodium-orthosilicate}}</ref>

==References==
{{reflist}}

Category:Silicon oxyanions
Category:Sorosilicates

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Adapted from the Wikipedia article [Pyrosilicate](https://en.wikipedia.org/wiki/Pyrosilicate) by Wikipedia contributors ([contributor history](https://en.wikipedia.org/wiki/Pyrosilicate?action=history)). Available under [Creative Commons Attribution-ShareAlike 4.0 International](https://creativecommons.org/licenses/by-sa/4.0/). Changes may have been made.
