kalinite
{{distinguish|kaolinite}}
{{Infobox mineral
| name = Kalinite
| category = Sulfate minerals
| boxwidth =
| boxbgcolor =
| image = Kalinite 1.jpg
| imagesize =
| caption = Kalinite from the Virgin Valley District, Nevada, USA. Specimen size 5.4 cm
| formula = KAl(SO4)2·11H2O
| molweight = 456.37 g/mol
| strunz = 7.CC.15
| dana = 29.5.4.2
| system = Monoclinic
| class = Prismatic (2/m)
(same H-M symbol)
| symmetry = C2/c
| unit cell = a = 19.92(16), b = 9.27(3)
c = 8.304(13) Å
β = 98.79(19)°; Z = 4
| color = White to pale blue
| habit = Fibrous
| lattice =
| twinning =
| cleavage =
| fracture = Conchoidal
| tenacity =
| mohs = 2 to 2.5
| luster = Vitreous
| refractive = nα = 1.429 to 1.430, nβ = 1.452, nγ = 1.456 to 1.458
| opticalprop = Biaxial (−)
| 2V = 52° (measured), 82° (calculated)
| birefringence = None
| pleochroism =
| streak = White
| gravity = 1.75 (observed) 2.0 (calculated)
| density =
| melt =
| fusibility =
| diagnostic =
| solubility = Soluble in water
| diaphaneity = Transparent
| other = Not fluorescent, barely detectable radioactivity| references = Gaines et al (1997) Dana’s New Mineralogy, Wiley[http://www.webmineral.com/data/Kalinite.shtml Kalinite on Webmin][http://www.mindat.org/min-2137.html Kalinite on Mindat]}}
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,American Mineralogist (1923) 8:15 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.{{Cite web|url=http://rruff.info/ima|title=IMA Mineral List with Database of Mineral Properties}} Many older samples, however, have been found to be potassium alum.[http://www.handbookofmineralogy.org/pdfs/kalinite.pdf Kalinite data in the Handbook of Mineralogy]
Environment
Kalinite is a rare secondary mineral observed in the oxidized zone of mineral deposits, as efflorescence on alum slates, in caves, and as a volcanic sublimate.American Mineralogist (1927) 12:14 It is associated with jarosite, KFe3+3(SO4)2(OH)6, and cuprian melanterite (pisanite), (Fe2+,Cu2+)SO4·7H2O, at Quetena, Chile.American Mineralogist (1938) 23:721