Description
The mineral calcite (also called limespar) consists primarily of the salt calcium carbonate (CaCO₃) and is one of the most abundant minerals in the Earth's crust. Calcium carbonate forms when soluble calcium ions come into contact with carbon dioxide and form a carbonate ion, provided a positive ion is present in the solution. Calcium carbonate is a sparingly soluble salt, causing the resulting CaCO₃ to precipitate; this occurs according to the following reaction: Ca²⁺(aq) + CO₃²⁻(aq) → CaCO₃(s). Calcite has a trigonal crystal system and belongs to the space group R-3c. A very pure form of calcite is also called bispar due to the double refraction of light in this mineral. It has a rhombohedral structure and is sometimes found as rhombohedral prisms, but it also frequently occurs in other forms, such as scalenohedra, or in fibrous, granular, or compact forms. The crystal structure is primarily a function of temperature, the degree of supersaturation in the crystal's immediate environment, and the CO₂ pressure. The calcite structure is the stable modification of CaCO₃ at room temperature. There is another form, aragonite, which transforms into calcite at 743 K. In its pure crystalline form, calcite is clear, colorless, and translucent, but due to impurities (such as copper or sodium salts), it can take on a variety of colors, including gray, blue, violet, green, and even black. It is often also opaque white. The mineral can exhibit both phosphorescence and fluorescence. Its hardness is defined as 3. Calcite is highly birefringent. This optical property was first described by Rasmus Bartholin when the Icelandic form of the mineral, consisting of large, crystal-clear rhombic rhombohedral plates, became available. Christiaan Huygens provided the first explanation with his wave theory of light. Calcite is a common constituent of sedimentary rocks, veins, and deposits in hot springs and caverns in karst regions (as stalactites). It is the mineral that forms limestone and thus the most common mineral of biological origin. Calcite is the main constituent of limestone, chalk, and marble, and is also a significant component of marl, calcareous sandstone, and limestone. Calcite is responsible for chemical weathering in igneous and metamorphic rocks, forming sedimentary rocks. Calcite is soluble in CO₂-containing water under slight pressure. As it falls into the air, rainwater absorbs the gaseous carbon dioxide, making it acidic. This acidic rainwater is capable of dissolving lime. Underground currents can transport this material in solution until, after contact with atmospheric pressure, CO₂ escapes and the calcite precipitates. This is how stalagmites and stalactites are formed in caves.
