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  2. Silicon dioxide - Wikipedia

    en.wikipedia.org/wiki/Silicon_dioxide

    Silicon dioxide is a relatively inert material (hence its widespread occurrence as a mineral). Silica is often used as inert containers for chemical reactions. At high temperatures, it is converted to silicon by reduction with carbon. Fluorine reacts with silicon dioxide to form SiF 4 and O 2 whereas the other halogen gases (Cl 2, Br 2, I 2 ...

  3. Coesite - Wikipedia

    en.wikipedia.org/wiki/Coesite

    Coesite (/ ˈ k oʊ s aɪ t /) [3] is a form of silicon dioxide (Si O 2) that is formed when very high pressure (2–3 gigapascals), and moderately high temperature (700 °C, 1,300 °F), are applied to quartz. Coesite was first synthesized by Loring Coes, Jr., a chemist at the Norton Company, in 1953. [4] [5]

  4. Structure of liquids and glasses - Wikipedia

    en.wikipedia.org/wiki/Structure_of_liquids_and...

    The attenuation of the peaks at increasing radial distances from the center indicates the decreasing degree of order from the center particle. This illustrates vividly the absence of "long-range order" in liquids and glasses. At long ranges, g(r) approaches a limiting value of 1, which corresponds to the macroscopic density of the material.

  5. Silicate mineral - Wikipedia

    en.wikipedia.org/wiki/Silicate_mineral

    In mineralogy, silica (silicon dioxide, SiO 2) is usually considered a silicate mineral rather than an oxide mineral. Silica is found in nature as the mineral quartz , and its polymorphs . On Earth, a wide variety of silicate minerals occur in an even wider range of combinations as a result of the processes that have been forming and re-working ...

  6. 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.

  7. Properties of water - Wikipedia

    en.wikipedia.org/wiki/Properties_of_water

    This attraction, hydrogen bonding, explains many of the properties of water, such as its solvent properties. [60] Although hydrogen bonding is a relatively weak attraction compared to the covalent bonds within the water molecule itself, it is responsible for several of the water's physical properties.

  8. Fused quartz - Wikipedia

    en.wikipedia.org/wiki/Fused_quartz

    The water content (and therefore infrared transmission) of fused quartz is determined by the manufacturing process. Flame-fused material always has a higher water content due to the combination of the hydrocarbons and oxygen fueling the furnace, forming hydroxyl [OH] groups within the material. An IR grade material typically has an [OH] content ...

  9. Hydrophobic silica - Wikipedia

    en.wikipedia.org/wiki/Hydrophobic_silica

    When applied to a surface of a material, the nanoparticles adhere to the host material and prevent liquids from permeating the rough texture. The water only comes into contact with the tips of the nanoparticles coating the outside of the material. Due to lack of attraction, the water is repelled from the hydrophobic silica. [3]