Hazenite

Phosphate mineral From Wikipedia, the free encyclopedia

Hazenite is a hydrous phosphate mineral with chemical formula of KNaMg2(PO4)2 · 14 H2O, therefore a hydrous alkali magnesium phosphate. It is a member of the struvite group.[4]

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Hazenite
General
CategoryPhosphate mineral
Struvite group
FormulaKNaMg2(PO4)2 · 14 H2O
IMA symbolHz[1]
Strunz classification8.CH.40
Dana classification40.01.01.03
Crystal systemOrthorhombic
Crystal classDipyramidal (mmm)
H–M Symbol: (2/m 2/m 2/m)
Space groupPmnb
Unit cella = 6.9349, b = 25.1737
c = 11.2189 [Å]; Z = 4
Identification
Formula mass276.331 g/mol
ColorColorless
Crystal habitRadiating elongated tabular or prismatic clusters or single bladed tabular crystals
Cleavage{001} Good
TenacityBrittle
Mohs scale hardness2 – 2.5
LusterVitreous
StreakWhite
DiaphaneityTransparent
Specific gravity1.91
Optical propertiesBiaxial (+)
Refractive indexnα =1.494(1), nβ = 1.498(1), nγ = 1.503(1)
2V angle41°
DispersionStrong r < v
SolubilityIn water
References[2][3][4]
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It was first described for an occurrence adjacent to Mono Lake, California, and named after Robert M. Hazen of the Carnegie Institute.[5] It was approved as a new mineral on February 28, 2008 by the Commission on New Minerals of the International Mineralogical Association.

It occurs as crystal clusters associated with decomposed cyanobacteria remnants on calcite or aragonite.[4] It is precipitated by microbes when the lake has been dry for so long that phosphorus levels build up, poisoning the microbes. They dispose of the excess phosphorus by excreting hazenite crystals.[6] The crystals disappear when it rains or the lake level rises.[7]

References

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