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Silicic acid
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In , a silicic acid () is any chemical compound containing the element attached to () and () groups, with the general formula or, equivalently, .

(2025). 9780080501093, Elsevier Science. .
(1979). 047102404X, Wiley. 047102404X
Orthosilicic acid is a representative example. Silicic acids are rarely observed in isolation, but are thought to exist in aqueous solutions, including , and play a role in biomineralization. They are typically colorless weak acids that are sparingly soluble in water. Like the anions, which are their better known , silicic acids are proposed to be or . No silicic acid has ever been identified, since these species are primarily of theoretical interest.

Depending on the number of silicon atoms present, there are mono- and polysilicic (di-, tri-, tetrasilicic, etc.) acids. Well defined silicic acids have not been obtained in a form that has been characterized by X-ray crystallography.


Examples


Reactions
Silicic acids can be seen as hydrated forms of silica, namely . Indeed, in concentrated solutions, silicic acids generally polymerize and condense, and ultimately degrade to silicon dioxide and . The intermediate stages may be very thick liquids or -like solids. Dehydrating the latter yields a hard translucent form of silica with atomic-scale pores, called , which is widely used as water absorbent and .

Silica dissolves very sparingly in water and is present in seawater at concentrations below 100 parts per million. In such dilute solutions, silica is assumed to exist as orthosilicic acid. Theoretical computations indicate that the dissolution of silica in water proceeds through the formation of a complex and then orthosilicic acid.

The silicon–oxygen double bond of metasilicic acid, implied by the formula , is hypothetical or highly unstable. Such double bonds can be hydrated to a pair of () groups:

=Si=O + H2O <-> =Si(-OH)2
For example,
\overset{metasilicic\ acid}{H2SiO3} + H2O <-> \overset{orthosilicic\ acid}{H4SiO4}
or
\overset{disilicic\ acid}{H2Si2O5} + 2 H2O <-> \overset{pyrosilicic\ acid}{(HO)3Si-O-Si(OH)3}
Alternatively, metasilicic acid is liable to form cyclic polymers , which can be opened by hydration to chain polymers . Similarly, disilicic acid is liable to form complex polymers with a tetravalent unit, . Conversely, and polymeric acids may depolymerize by of the bridges, or such bridges may be created by condensation:
#Si-O-Si# + H2O <-> #Si-OH + HO-Si#

Like organic , silicic acids are weak acids. Orthosilicic acid has calculated dissociation potentials p K = 9.84, p K = 13.2 at 25 °C.

Silicic acids and silicates in solution react with anions, yielding yellow complexes. This reaction has been used to the content of silicon in water solutions and determine their nature. In a typical preparation, orthosilicic acid was found to react completely in 75 seconds, dimeric pyrosilicic acid in 10 minutes, and higher in considerably longer time. The reaction is not observed with .

The degree of polymerization of silicic acids in water solution can be determined by its effect on the of the solution ().


History
Silicic acid was invoked by Jöns Jacob Berzelius in the early 19th century to explain the dissolution of (silica, quartz) in water, namely through the hydration reaction:
\overset{silica}{SiO2} + \overset{water}{H2O} <-> \overset{silicic\ acid}{H2SiO3}

Based on the curves for , Reinout Willem Van Bemmelen argued that no hydrates existed, only silica gel. On the other hand, Gustav Tschermak von Seysenegg believed that he had observed different silicic acids as decomposition products of gels..

The first crystalline silicic acid was prepared from the () in 1924. More than 15 crystalline acids are known and comprise at least six modifications of . Some acids can and intercalate organic molecules, and therefore are interesting alternatives to silica..


Preparation
Crystalline silicic acids can be prepared by removing the sodium cations from solutions of with an ion-exchange resin, or by treating with concentrated .


See also

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