Kainite
Kainite | |
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Kainite | |
General | |
Category | Sulfate minerals |
Formula (repeating unit) | KMg(SO4)Cl·3H2O |
Strunz classification | 07.DF.10 |
Crystal symmetry |
Monoclinic prismatic H-M symbol: (2/m) Space group: C 2/m |
Unit cell | a = 19.72 Å, b = 16.23 Å, c = 9.53 Å; β = 94.92° |
Identification | |
Color | Colorless; yellow, brownish, greyish-green, red, violet, blue |
Crystal habit | Crystal aggregates, fibrous, massive |
Crystal system | Monoclinic |
Cleavage | {001}, perfect |
Fracture | Splintery |
Tenacity | Brittle |
Mohs scale hardness | 2.5-3 |
Luster | Vitreous |
Streak | White |
Diaphaneity | Transparent |
Specific gravity | 2.15 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.494 nβ = 1.505 nγ = 1.516 |
Birefringence | δ = 0.022 |
Pleochroism | Visible: X = violet, Y = blue, Z = yellowish |
2V angle | Measured: 90° |
Dispersion | Weak |
References | [1][2][3] |
Kainite (KMg(SO4)Cl·3H2O) is a mineral salt that consists of potassium chloride and magnesium sulfate and is used as a fertilizer. This mineral is dull and soft, is colored white through yellow to red and is found in the Stassfurt salt mines in Saxony, Germany. It is a natural salt occurring in irregular granular masses, and is used as a source of potassium and magnesium compounds.