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  2. Lime kiln - Wikipedia

    en.wikipedia.org/wiki/Lime_kiln

    Rotary lime kiln (rust-colored horizontal tube at right) with preheater, Wyoming, 2010 Traditional lime kiln in Sri Lanka. A lime kiln is a kiln used for the calcination of limestone (calcium carbonate) to produce the form of lime called quicklime (calcium oxide). The chemical equation for this reaction is CaCO 3 + heat → CaO + CO 2

  3. Calcination - Wikipedia

    en.wikipedia.org/wiki/Calcination

    In limestone calcination, a decomposition process that occurs at 900 to 1050 °C, the chemical reaction is CaCO 3 (s) → CaO(s) + CO 2 (g) Today, this reaction largely occurs in a cement kiln. The standard Gibbs free energy of reaction in [J/mol] is approximated as ΔG° r ≈ 177,100 J/mol − 158 J/(mol*K) * T. [4]

  4. Limepit - Wikipedia

    en.wikipedia.org/wiki/Limepit

    The limestone blocks were then crushed, afterwards slaked (the process of adding water and constantly turning the lime to create a chemical reaction, whereby the burnt lime, or what is known also as calcium oxide, [7] is changed into calcium hydroxide), and mixed with an aggregate to form an adhesive paste (plaster) used in construction and for ...

  5. Liming (soil) - Wikipedia

    en.wikipedia.org/wiki/Liming_(soil)

    Prepared agricultural lime staged near a field in the UK. Liming is the application of calcium- (Ca) and magnesium (Mg)-rich materials in various forms, including marl, chalk, limestone, burnt lime or hydrated lime to soil. [1] In acid soils, these materials react as a base and neutralize soil acidity.

  6. Carbonate rock - Wikipedia

    en.wikipedia.org/wiki/Carbonate_rock

    Limestone is the most common carbonate rock [3] and is a sedimentary rock made of calcium carbonate with two main polymorphs: calcite and aragonite.While the chemical composition of these two minerals is the same, their physical properties differ significantly due to their different crystalline form.

  7. Recrystallization (geology) - Wikipedia

    en.wikipedia.org/wiki/Recrystallization_(geology)

    In geology, solid-state recrystallization is a metamorphic process that occurs under high temperatures and pressures where atoms of minerals are reorganized by diffusion and/or dislocation glide. During this process, the physical structure of the minerals is altered while the composition remains unchanged.

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  9. Decrepitation - Wikipedia

    en.wikipedia.org/wiki/Decrepitation

    Decrepitation is one of the most accurate ways to calculate a mineral-deposit scale so that the analysis of the hydrothermal system is advanced and improved. Fluid inclusions are important in regard to decrepitation because they are the microscopic areas of gas and liquid within crystals that are decrepitated, or broken, with the application of heat.