Today we want to talk about Blödite. Blödite is a topic that has sparked the interest of many people in recent times. Its relevance has transcended borders and has become a source of debate and reflection in different spheres of society. Many experts have dedicated time and effort to studying Blödite, seeking to understand its impact and scope in our daily lives. In this article, we will explore different aspects related to Blödite, from its origin to its possible future implications. We hope this reading provides a comprehensive view on Blödite and its implications in today's society.
Blödite | |
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![]() Doubly terminated blödite crystal from Soda Lake, San Luis Obispo County, California (size: 7.0 × 4.8 × 1.9 cm) | |
General | |
Category | Sulfate minerals |
Formula | Na2Mg(SO4)2·4H2O |
IMA symbol | Blö[1] |
Strunz classification | 7.CC.50 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P21/a |
Unit cell | a = 11.04 Å, b = 8.15 Å, c = 5.49 Å; β = 100.41°; Z = 2 |
Identification | |
Color | Colorless, yellow, may be dark gray, bluish green, or reddish due to inclusions |
Crystal habit | Prismatic to equant crystals, granular, massive |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 2.5–3 |
Luster | Vitreous |
Specific gravity | 2.23 |
Optical properties | Biaxial (−) |
Refractive index | nα = 1.483, nβ = 1.486, nγ = 1.487 |
Birefringence | δ = 0.004 |
2V angle | 71° (measured) |
References | [2][3][4] |
Blödite or bloedite is a hydrated sodium magnesium sulfate mineral with the formula Na2Mg(SO4)2·4H2O. The mineral is clear to yellow in color often darkened by inclusions and forms monoclinic crystals.
Blödite was first described in 1821 for an occurrence in a salt deposit in Ischler Salzberg, Bad Ischl, Gmunden, Austria and named for German mineralogist and chemist Karl August Blöde (1773–1820).[3][4]
It is found worldwide in evaporitic sedimentary environments such as the Great Salt Lake, Utah.