User:Strickja/Kalinite

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{{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

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