Calcite
Calcium carbonate mineral / From Wikipedia, the free encyclopedia
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Calcite is a carbonate mineral and the most stable polymorph of calcium carbonate (CaCO3). It is a very common mineral, particularly as a component of limestone. Calcite defines hardness 3 on the Mohs scale of mineral hardness, based on scratch hardness comparison. Large calcite crystals are used in optical equipment, and limestone composed mostly of calcite has numerous uses.
Quick Facts General, Category ...
Calcite | |
---|---|
General | |
Category | Carbonate mineral |
Formula (repeating unit) | CaCO3 |
Strunz classification | 5.AB.05 |
Crystal system | Trigonal |
Crystal class | Hexagonal scalenohedral (3m) H-M symbol: (3 2/m) |
Space group | R3c |
Unit cell | a = 4.9896(2) Å, c = 17.0610(11) Å; Z = 6 |
Identification | |
Color | Typically colorless or creamy white - may have shades of brownish colors |
Crystal habit | Botryoidal, concretionary, druse, globular, granular, massive, rhombohedral, scalenohedral, stalactitic |
Twinning | Common by four twin laws |
Cleavage | Perfect on {1011} three directions with angle of 74° 55'[1] |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 3 (defining mineral) |
Luster | Vitreous to pearly on cleavage surfaces |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | 2.71 |
Optical properties | Uniaxial (−); low relief |
Refractive index | nω = 1.640–1.660 nε = 1.486 |
Birefringence | δ = 0.154–0.174 |
Fusibility | Infusible (decrepitates energetically)[2] |
Solubility | Soluble in dilute acids |
Other characteristics | May fluoresce red, blue, yellow, and other colors under either SW and LW UV; phosphorescent |
References | [3][4][5] |
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Other polymorphs of calcium carbonate are the minerals aragonite and vaterite. Aragonite will change to calcite over timescales of days or less at temperatures exceeding 300 °C,[6][7] and vaterite is even less stable.