Chalcopyrite | |
---|---|
General | |
Category | Sulfide mineral |
Formula (repeating unit) | CuFeS2 |
IMA symbol | Ccp[1] |
Strunz classification | 2.CB.10a |
Crystal system | Tetragonal |
Crystal class | Scalenohedral (42m) H-M symbol: (4 2m) |
Space group | I42d |
Unit cell | a = 5.289 Å, c = 10.423 Å; Z = 4 |
Identification | |
Formula mass | 183.54 g/mol |
Color | Brass yellow, may have iridescent purplish tarnish. |
Crystal habit | Predominantly the disphenoid and resembles a tetrahedron, commonly massive, and sometimes botryoidal. |
Twinning | Penetration twins |
Cleavage | Indistinct on {011} |
Fracture | Irregular to uneven |
Tenacity | Brittle |
Mohs scale hardness | 3.5–4 |
Luster | Metallic |
Streak | Greenish black |
Diaphaneity | Opaque |
Specific gravity | 4.1–4.3 |
Optical properties | Opaque |
Solubility | Soluble in HNO3 |
Other characteristics | magnetic on heating |
References | [2][3][4][5][6] |
Chalcopyrite (/ˌkælkəˈpaɪˌraɪt, -koʊ-/[7][8] KAL-kə-PY-ryte, -koh-) is a copper iron sulfide mineral and the most abundant copper ore mineral. It has the chemical formula CuFeS2 and crystallizes in the tetragonal system. It has a brassy to golden yellow color and a hardness of 3.5 to 4 on the Mohs scale. Its streak is diagnostic as green-tinged black.[9]
On exposure to air, chalcopyrite tarnishes to a variety of oxides, hydroxides, and sulfates. Associated copper minerals include the sulfides bornite (Cu5FeS4), chalcocite (Cu2S), covellite (CuS), digenite (Cu9S5); carbonates such as malachite and azurite, and rarely oxides such as cuprite (Cu2O). It is rarely found in association with native copper. Chalcopyrite is a conductor of electricity.[10]
Copper can be extracted from chalcopyrite ore using various methods. The two predominant methods are pyrometallurgy and hydrometallurgy, the former being the most commercially viable.[11]
Daehn-2022
was invoked but never defined (see the help page).