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  2. Silicate mineral paint - Wikipedia

    en.wikipedia.org/wiki/Silicate_mineral_paint

    Silicate mineral paint. Silicate mineral paints or mineral colors are paint coats with mineral binding agents. Two relevant mineral binders play a role in the field of colors: Lime and silicate. Under influence of carbon dioxide, lime-based binders carbonate and water silicate-based binders solidify. Together they form calcium silicate hydrates.

  3. Sodium silicate - Wikipedia

    en.wikipedia.org/wiki/Sodium_silicate

    Sodium silicate glass-to-glass bonding has the advantage that it is a low-temperature bonding technique, as opposed to fusion bonding. [21] It also requires less processing than glass-to-glass anodic bonding, [ 23 ] which requires an intermediate layer such as silicon nitride (SiN) to act as a diffusion barrier for sodium ions. [ 23 ]

  4. Substrate (materials science) - Wikipedia

    en.wikipedia.org/wiki/Substrate_(materials_science)

    In materials science and engineering, a substrate refers to a base material on which processing is conducted. This surface could be used to produce new film or layers of material such as deposited coatings. It could be the base to which paint, adhesives, or adhesive tape is bonded. A typical substrate might be rigid such as metal, concrete, or ...

  5. Tin - Wikipedia

    en.wikipedia.org/wiki/Tin

    Tin. Tin is a chemical element; it has symbol Sn (from Latin stannum) and atomic number 50. A silvery-colored metal, tin is soft enough to be cut with little force, [10] and a bar of tin can be bent by hand with little effort. When bent, the so-called "tin cry" can be heard as a result of twinning in tin crystals. [11]

  6. Mineral painting - Wikipedia

    en.wikipedia.org/wiki/Mineral_painting

    Mineral painting or Keim's process, also known as stereochromy, is a mural or fresco painting technique that uses a water glass -based paint to maximize the lifetime of the finished work. The name "stereochromy" was first used in about 1825 by Johann Nepomuk von Fuchs and Schlotthaurer. [1] In the original technique, pigments were applied to ...

  7. Cristobalite - Wikipedia

    en.wikipedia.org/wiki/Cristobalite

    Cristobalite spherulites formed by devitrification from the obsidian matrix. Specimen from California, US; size: 5.9 cm × 3.8 cm × 3.8 cm (2.3 in × 1.5 in × 1.5 in). Cristobalite (/ krɪˈstoʊbəˌlaɪt /) is a mineral polymorph of silica that is formed at very high temperatures. It has the same chemical formula as quartz, SiO 2, but a ...

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