Blossite
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| Blossite | |
|---|---|
| General | |
| Category | Vanadate mineral |
| Formula | CuV2O7 |
| IMA symbol | Blo[1] |
| Strunz classification | 8.FA.05 |
| Dana classification | 38.5.6.1 |
| Crystal system | Orthorhombic |
| Crystal class | Pyramidal (mm2) (same H-M symbol) |
| Space group | Fdd2 |
| Unit cell | a = 20.676(6) Å, b = 8.392(3) Å, c = 6.446(2) Å; Z = 8 |
| Identification | |
| Color | Black, white in reflected light, red-brown internal reflections |
| Crystal habit | Anhedral crystals and intergrowths |
| Luster | Metallic |
| Streak | Red brown |
| Diaphaneity | Opaque |
| Specific gravity | 3.95 – 3.97 (measured on synthetic material) 4.05 (calculated) |
| Optical properties | Biaxial |
| Refractive index | 2.05 |
| Birefringence | Bireflectance: weak to moderate: cream-white shades |
| References | [2][3][4] |
Blossite is an anhydrous copper vanadate mineral with the formula: Cu2+V5+2O7.[5] Blossite was named for mineralogist F. Donald Bloss of Virginia Polytechnic Institute and State University.[6]
Blossite was first described for an occurrence in the “Y” fumarole[7] in the summit crater of Izalco Volcano, El Salvador.[6] There it occurs with several high-temperature minerals including: stoiberite, fingerite, ziesite, and mcbirneyite.[6] The natural analogues of these compounds crystallize in the CuO-V2O5 binary system first studied by Brisi and Molinari (1958) and were first discovered as synthetic compounds. Blossite is the low temperature polymorph of ziesite, β-Cu2V2O7.[6] All of the blossite crystals identified to date are inter-grown[6] with other fumarolic copper vanadates. The discovered location of these copper vanadates, in the outer sulfate zone of the fumarole, indicates a sublimation temperature between 100 °C and 200 °C.[8]
Physical properties
Blossite occurs as black anhedral crystals, with dimensions not exceeding 150 um. Crystals of blossite have only been isolated with other fumarolic copper vanadates or sulfates. Blossite demonstrates a red-brown streak, prevalent to the natural copper present, this red-brown coloring is also a prevalent in the internal reflections. No cleavage is observed in blossite, but the size of the natural mineral grains of polycrystalline prohibit the identification of cleavage. In ultraviolet radiation blossite does not fluoresce, it demonstrates a white color when blue-filtered white light in air is present, and is opaque to transmitted light. The density of natural occurring blossite is 4.051 g/cm3.[6]