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  2. Silicic acid - Wikipedia

    en.wikipedia.org/wiki/Silicic_acid

    This reaction has been used to titrate the content of silicon in water solutions and determine their nature. In a typical preparation, monomeric orthosilicic acid was found to react completely in 75 seconds, dimeric pyrosilicic acid in 10 minutes, and higher oligomers in considerably longer time. The reaction is not observed with colloidal ...

  3. Hydrated silica - Wikipedia

    en.wikipedia.org/wiki/Hydrated_silica

    Hydrated silica is a form of silicon dioxide, which has a variable amount of water in the formula. When dissolved in water, it is usually known as silicic acid. It is found in nature as opal [2] (which has been mined as a gemstone for centuries), and in the cell walls of diatoms.

  4. Alkali–silica reaction - Wikipedia

    en.wikipedia.org/wiki/Alkali–silica_reaction

    The alkali-silica reaction mechanism catalysed by a soluble strong base as NaOH or KOH in the presence of Ca(OH) 2 (alkalinity buffer present in the solid phase) can be compared with the carbonatation process of soda lime. The silicic acid (H 2 SiO 3 or SiO 2) is simply replaced in the reaction by the carbonic acid (H 2 CO 3 or CO 2).

  5. Silica cycle - Wikipedia

    en.wikipedia.org/wiki/Silica_cycle

    [5] [6] It results in the generation of silicic acid in aqueous environments. Silicic acid, Si(OH) 4, is a hydrated form of silica found only as an unstable solution in water, yet it plays a central role in the silica cycle. [1] Silicifiers are organisms that use silicic acid to precipitate biogenic silica, SiO 2.

  6. Pozzolanic activity - Wikipedia

    en.wikipedia.org/wiki/Pozzolanic_activity

    Pozzolanic reaction is a long term reaction, which involves dissolved silicic acid, water and CaO or Ca(OH) 2 or other pozzolans to form a strong cementation matrix. This process is often irreversible. Sufficient amount of free calcium ion and a high pH of 12 and above is needed to initiate and maintain the pozzolanic reaction. [2]

  7. Silicification - Wikipedia

    en.wikipedia.org/wiki/Silicification

    Silicic acid (H 4 SiO 4) in the silica-enriched fluids forms lenticular, nodular, fibrous, or aggregated quartz, opal, or chalcedony that grows within the rock. [5] Silicification happens when rocks or organic materials are in contact with silica-rich surface water, buried under sediments and susceptible to groundwater flow, or buried under ...

  8. Colloidal silica - Wikipedia

    en.wikipedia.org/wiki/Colloidal_silica

    The subunits of colloidal silica particles are typically in the range of 1 to 5 nm. Whether or not these subunits are joined depends on the conditions of polymerization. Initial acidification of a water-glass (sodium silicate) solution yields Si(OH) 4. If the pH is reduced below 7 or if salt is added, then the units tend to fuse together in chains.

  9. Orthosilicic acid - Wikipedia

    en.wikipedia.org/wiki/Orthosilicic_acid

    2009 silicic acid concentration in the upper pelagic zone. [19] Dissolved silica (DSi) is a term used in the field of oceanography to describe the form of water-soluble silica, which is assumed to be Si(OH) 4 (orthosilicic acid) or its conjugate bases (orthosilicate anions) such as − O−Si(OH) 3 and (− O−) 2 Si(OH) 2.

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