Langbeinite
Langbeinite is a potassium magnesium sulfate mineral with the chemical formula K2Mg2(SO4)3. Langbeinite crystallizes in the isometric-tetartoidal (cubic) system as transparent colorless or white with pale tints of yellow to green and violet crystalline masses. It has a vitreous luster. The Mohs hardness is 3.5 to 4 and the specific gravity is 2.83. The crystals are piezoelectric.[2]
Langbeinite | |
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Langbeinite in the History Museum, Truskavets | |
General | |
Category | Sulfate mineral |
Formula (repeating unit) | K2Mg2(SO4)3 |
Strunz classification | 7.AC.10 |
Crystal system | Cubic |
Crystal class | Tetartoidal (23) (same H-M symbol) |
Space group | P213 |
Unit cell | a = 9.92 Å; Z = 4 |
Identification | |
Color | Colorless with pale shades of yellow, pink, red, green, gray |
Crystal habit | As nodules, disseminated grains, bedded massive |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 3.5 - 4 |
Luster | Vitreous |
Diaphaneity | Transparent |
Specific gravity | 2.83 |
Optical properties | Isotropic |
Refractive index | n = 1.5329–1.5347 |
Solubility | 240 g/L (20°C);[1] Slowly dissolves in water |
Other characteristics | Piezoelectric |
References | [2][3][4] |
The mineral is an ore of potassium and occurs in marine evaporite deposits in association with carnallite, halite and sylvite.[2]
It was first described in 1891 for an occurrence in Wilhelmshall, Halberstadt, Saxony-Anhalt, Germany, and named for A. Langbein of Leopoldshall, Germany.[2][3]
Langbeinite gives its name to the langbeinites, a family of substances with the same cubic structure, a tetrahedral anion, and large and small cations.
Related substances include hydrated salts leonite (K2Mg(SO4)2·4H2O) and picromerite (K2Mg(SO4)2·6H2O).