Chrysotile | |
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General | |
Category | Phyllosilicates Kaolinite-serpentine group |
Formula (repeating unit) | Mg3(Si2O5)(OH)4 (ideal) |
IMA symbol | Ctl[1] |
Strunz classification | 9.ED.15 |
Crystal system | Monoclinic: clinochrysotile (most common) Orthorhombic: orthochrysotile and parachrysotile (both rare) |
Crystal class | Clinochrysotile: prismatic (2/m) Orthochrysotile and parachrysotile: pyramidal (mm2) |
Space group | Clinochrysotile: C2/m Orthochrysotile and parachrysotile: Ccm21 |
Identification | |
Formula mass | 277.11 g/mol (ideal) |
Colour | White to greyish green |
Crystal habit | Acicular |
Fracture | Fibrous |
Mohs scale hardness | 2.5–3 |
Lustre | Silky |
Streak | White |
Diaphaneity | Translucent |
Density | 2.53 g/ml |
Optical properties | Biaxial (+) |
Refractive index | nα = 1.569, nγ = 1.570 |
Birefringence | 0.001 (max) |
Dispersion | Relatively weak |
Extinction | parallel |
Melting point | 600–850 °C (1,112–1,562 °F) (decomposes) |
Fusibility | dehydrates at 550–750 °C (1,022–1,382 °F) |
Diagnostic features | White to grayish green thin, flexible curved fiber |
Solubility | Insoluble in water Fibres degrade in dilute acid |
References | [2][3][4] |
Chrysotile or white asbestos is the most commonly encountered form of asbestos,[5] accounting for approximately 95% of the asbestos in the United States[6] and a similar proportion in other countries.[7] It is a soft, fibrous silicate mineral in the serpentine subgroup of phyllosilicates; as such, it is distinct from other asbestiform minerals in the amphibole group. Its idealized chemical formula is Mg3(Si2O5)(OH)4.[5] The material has physical properties which make it desirable for inclusion in building materials, but poses serious health risks when dispersed into air and inhaled.