In chemistry, a silicic acid () is any chemical compound containing the element silicon attached to oxide () and hydroxyl () groups, with the general formula or, equivalently, .
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.
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 hydroxyl () groups:
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 molybdate anions, yielding yellow silicomolybdate complexes. This reaction has been used to titration 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 colloidal silica.
The degree of polymerization of silicic acids in water solution can be determined by its effect on the freezing point of the solution (cryoscopy).
Based on the vapor pressure curves for silica gel, Reinout Willem Van Bemmelen argued that no silica 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 Phyllosilicate gels..
The first crystalline silicic acid was prepared from the phyllosilicate natrosilite () in 1924. More than 15 crystalline acids are known and comprise at least six modifications of . Some acids can adsorption and intercalate organic molecules, and therefore are interesting alternatives to silica..
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