User:Strickja/Kalinite
{{Userspace draft|source=ArticleWizard|date=March 2010}}
{{Infobox mineral
| name = Kalinite
| category = Sulfate Mineral
| boxwidth = 24
| boxbgcolor =
| image = Kalinite 1.jpg
| caption = Kalinite from the Virgin Valley District, Nevada, USA. Specimen size 5.4 cm
| formula = KAl(SO4)2.11H2O
| molweight = 456.37 g
| strunz = 6/C.13-20 or 7.CC.15
| dana = 29.5.4.2
| color = White to pale blue
| habit = Fibrous
| system = Monoclinic 2/m prismatic
| 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 = http://www.webmineral.com/data/Kalinite.shtmlhttp://www.mindat.org/min-2137.html}}
Kalinite is a fibrous monoclinic type of alum distinct from isometric potassium alumAmerican Mineralogist (1923) 8:15, named in 1868 for its potassium content. Kalium is the Latin name for potassium (hence its chemical symbol, "K").
A proposal to discredit kalinite as a mineral species has been submitted to the International Mineralogical Association, but it is currently (March 2010) on the list of approved mineralshttp://rruff.info/ima. Many older samples, however, have been found to be potassium alumhttp://www.handbookofmineralogy.org/pdfs/kalinite.pdf.
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 sublimateAmerican 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, ChileAmerican Mineralogist (1938) 23:721.
Unit Cell
Space Group: C2/c
Unit Cell ParametersGaines et al (1997) Dana’s New Mineralogy, Wiley: a=19.92 Å, b=9.27 Å, c=8.304 Å, β = 98.79°, Z=4
References
{{Reflist}}