Kalinite
| Kalinite | |
|---|---|
| Kalinite from the Virgin Valley District, Nevada, USA.  Specimen size 5.4 cm | |
| General | |
| Category | Sulfate minerals | 
| Formula | KAl(SO4)2·11H2O | 
| IMA symbol | Kli | 
| Strunz classification | 7.CC.15 | 
| Dana classification | 29.5.4.2 | 
| Crystal system | Monoclinic | 
| Crystal class | Prismatic (2/m) (same H-M symbol) | 
| Space group | C2/c | 
| Unit cell | a = 19.92(16), b = 9.27(3) c = 8.304(13) Å β = 98.79(19)°; Z = 4 | 
| Identification | |
| Formula mass | 456.37 g/mol | 
| Color | White to pale blue | 
| Crystal habit | Fibrous | 
| Fracture | Conchoidal | 
| Mohs scale hardness | 2 to 2.5 | 
| Luster | Vitreous | 
| Streak | White | 
| Diaphaneity | Transparent | 
| Specific gravity | 1.75 (observed) 2.0 (calculated) | 
| Optical properties | Biaxial (−) | 
| Refractive index | nα = 1.429 to 1.430, nβ = 1.452, nγ = 1.456 to 1.458 | 
| Birefringence | None | 
| 2V angle | 52° (measured), 82° (calculated) | 
| Solubility | Soluble in water | 
| Other characteristics | Not fluorescent, barely detectable radioactivity | 
| References | |
Kalinite is a mineral composed of hydrated potassium aluminium sulfate (a type of alum). It is a fibrous monoclinic alum, distinct from isometric potassium alum, named in 1868. Its name comes from kalium (derived from Arabic: القَلْيَه al-qalyah "plant ashes", which is the Latin name for potassium, hence its chemical symbol, "K".
A proposal to remove recognition of kalinite as a mineral species was submitted to the International Mineralogical Association; however, kalinite is still on the list of approved minerals. Many older samples, however, have been found to be potassium alum.