Kernite
| Kernite | |
|---|---|
| General | |
| Category | Inoborates |
| Chemical formula | Na2B4O6(OH)2·3(H2O) |
| Strunz classification | 06.DB.05 |
| Identification | |
| Molar mass | 290.28 |
| Color | Colorless, white |
| Crystal habit | Crystalline - Coarse - Occurs as well-formed coarse sized crystals |
| Crystal system | Monoclinic, (2/m) Space Group P 21/c |
| Cleavage | [100] Perfect, [001] Perfect, [201] Good |
| Fracture | Brittle - Generally displayed by glasses and most non-metallic minerals |
| Mohs scale hardness | 2.5-3 |
| Luster | Vitreous - Pearly |
| Streak | white |
| Specific gravity | 1.9 - 1.92, Average = 1.91 |
| Optical properties | Biaxial (-), 2V=80 |
| Refractive index | nα=1.454, nβ=1.472, nγ=1.488 |
| Birefringence | δ =0.0340 |
| Other characteristics | non-radioactive, non-fluorescent, non-magnetic |
| References | [1] |
Kernite, also known as rasorite is a hydrated sodium borate hydroxide mineral with formula Na2B4O6(OH)2·3H2O. It is a colorless to white mineral crystallizing in the monoclinic crystal system typically occurring as prismatic to acicular crystals or granular masses. It is relatively soft with Mohs hardness of 2.5 to 3 and light with a specific gravity of 1.91. It exhibits perfect cleavage and a brittle fracture. Kernite is used to produce borax which can be used in a variety of soaps.
The mineral was discovered in 1926 in Kern County, California and later named for the county. Kern County was the only known source of kernite for many years, but kernite is now also mined in Argentina, Spain, and Turkey. It occurs in sedimentary evaporite deposits in arid regions. The largest documented single crystal of kernite measured 2.44x0.9x0.9 m3 and weighed ~3.8 tons.[2]
[edit] References
- ^ Kernite WebMineral
- ^ P. C. Rickwood (1981). "The largest crystals". American Mineralogist 66: 885–907. http://www.minsocam.org/ammin/AM66/AM66_885.pdf.
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