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Carbonate mineral,

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any kind of member of a family members of minerals the contain the carbonate ion, CO32-, as the an easy structural and also compositional unit. The carbonates are amongst the many widely dispersed minerals in the earth’s crust.

The crystal framework of many carbonate minerals reflects the trigonal symmetry of the carbonate ion, i beg your pardon is written of a carbon atom centrally located in an it is provided triangle the oxygen atoms. This anion team usually wake up in mix with calcium, sodium, uranium, iron, aluminum, manganese, barium, zinc, copper, lead, or the rare-earth elements. The carbonates have tendency to it is in soft, dissolve in hydrochloric acid, and have a significant anisotropy in plenty of physical nature (e.g., high birefringence) as a an outcome of the planar framework of the lead carbonate ion.



The lead carbonate minerals save on computer the anionic facility (CO3)2–, i m sorry is triangle in that coordination—i.e., v a carbon...

There are about 80 recognized carbonate minerals, but most the them are rare. The commonest varieties, calcite, dolomite, and aragonite, are influential constituents of certain rocks: calcite is the principal mineral of limestones and marbles; dolomite occurs together a replacement because that calcite in limestones, and when this is considerable the absent is termed dolomite; and aragonite wake up in some recent sediments and also in the shells of biology that have actually calcareous skeletons. Other fairly common carbonate minerals serve as steel ores: siderite, for iron; rhodochrosite, because that manganese; strontianite, because that strontium; smithsonite, for zinc; witherite, because that barium; and also cerussite, for lead.

Most together rock-forming carbonates belong to one of two structure groups—either calcite or aragonite. The calcite framework is usually described with recommendation to the salt chloride structure in i m sorry the sodium and chloride of halite are changed by calcium atoms and CO3 groups, respectively. The unit cabinet of halite is distorted by compression along a three-fold axis, causing a rhombohedral cell. In calcite all CO3 groups are parallel and lie in horizontal layers; CO3 teams in nearby layers, however, point in the contrary directions. The calcium atoms room bonded to six oxygen atoms, one every from 3 CO3 teams in a layer above and three from CO3 groups in a class below. The framework of dolomite, CaMg(CO3)2, is similar to that of calcite, CaCO3, other than that over there is constant alternation that calcium and magnesium, and also a lower symmetry, though still rhombohedral, results. The 2nd structure group, the of aragonite, is orthorhombic. Favor the calcite structure, the cation in the aragonite structure is surrounded by 6 carbonate groups; the CO3 groups, however, are rotated around an axis perpendicular to their plane and the cation is combination to ripe oxygen atoms instead of six.

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Carbonate minerals other than an easy carbonates include hydrated carbonates, bicarbonates, and also compound carbonates containing other anions in addition to carbonate. The very first two groups incorporate nahcolite, trona, natron, and also shortite; they typically occur in sedimentary evaporite deposits and as low-temperature hydrothermal modification products. The members of the 3rd group normally contain rare-earth aspects and virtually always an outcome from hydrothermal alteration at low temperatures. Instances of these carbonate minerals room bastnäsite, doverite, malachite, and also azurite.