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  2. Silicon dioxide - Wikipedia

    en.wikipedia.org/wiki/Silicon_dioxide

    As it does not contain any hydrogen, non-hydrated silica cannot directly act as a Brønsted–Lowry acid. While silicon dioxide is only poorly soluble in water at low or neutral pH (typically, 2 × 10 −4 M for quartz up to 10 −3 M for cryptocrystalline chalcedony), strong bases react with glass and easily dissolve it. Therefore, strong ...

  3. Silica cycle - Wikipedia

    en.wikipedia.org/wiki/Silica_cycle

    The silica cycle plays an important role in long term global climate regulation. The global silica cycle also has large effects on the global carbon cycle through the carbonate-silicate cycle. [43] The process of silicate mineral weathering transfers atmospheric CO 2 to the hydrologic cycle through the chemical reaction displayed above. [4]

  4. Colloidal silica - Wikipedia

    en.wikipedia.org/wiki/Colloidal_silica

    Colloidal silicas are most often prepared in a multi-step process where an alkali-silicate solution is partially neutralized, leading to the formation of silica nuclei. 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.

  5. Silicic acid - Wikipedia

    en.wikipedia.org/wiki/Silicic_acid

    [4] [5] [6] Dehydrating the latter yields a hard translucent form of silica with atomic-scale pores, called silica gel, which is widely used as water absorbent and drying agent. Silica dissolves very sparingly in water [citation needed] and is present in seawater at concentrations below 100 parts per million. In such dilute solutions, silica is ...

  6. Carbonate–silicate cycle - Wikipedia

    en.wikipedia.org/wiki/Carbonate–silicate_cycle

    Carbonic acid is a weak acid, but over long timescales, it can dissolve silicate rocks (as well as carbonate rocks). Most of the Earth's crust (and mantle) is composed of silicates. [8] These substances break down into dissolved ions as a result.

  7. Sodium silicate - Wikipedia

    en.wikipedia.org/wiki/Sodium_silicate

    The fixing type was "a mixture of silica well saturated with potash water glass and a sodium silicate" used to stabilize inorganic water color pigments on cement work for outdoor signs and murals. [12] [13] [14] [15]

  8. Silicification - Wikipedia

    en.wikipedia.org/wiki/Silicification

    Lithological silica are brought to surface through volcanic events whereas weathering of pre-existing rocks releases silica into the waters. The sources of silica can be divided into two categories: silica in organic and inorganic materials. The former category is also known as biogenic silica, which is a ubiquitous material in animals and plants.

  9. 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 .