Plumbogummite
| Plumbogummite | |
|---|---|
|
Plumbogummite from the Yangshuo Mine, Guangxi Province, China. Specimen size 4 cm. | |
| General | |
| Category | Phosphate minerals |
| Formula (repeating unit) | PbAl3(PO4)2(OH)5·H2O |
| Strunz classification | 08.BL.10 |
| Dana classification | 42.7.3.5 |
| Identification | |
| Formula mass | 581.14 g |
| Color | Blue, grey, greenish or yellow |
| Crystal habit | Crystals, rare, have a hexagonal outline |
| Crystal system | Trigonal – Hexagonal Scalenohedral, 3 2/m |
| Cleavage | None |
| Fracture | Uneven or sub-conchoidal |
| Tenacity | Brittle |
| Mohs scale hardness | 4 to 5 [1][2] or 4.5 to 5[3][4] |
| Luster | Resinous or dull |
| Streak | White |
| Diaphaneity | Translucent |
| Specific gravity | 4.014 |
| Optical properties | Uniaxial (+), segments of crystals may be biaxial[4] |
| Refractive index |
no = 1.653[3] or 1.653 to 1.688[4] |
| Pleochroism | None[5] |
| Solubility | Soluble in hot acids |
| Other characteristics | Non-fluorescent, not radioactive |
| References | [1][2][3][4] |
Plumbogummite is a rare secondary lead phosphate mineral, belonging to the alunite supergroup of minerals, crandallite subgroup.[1] Some other members of this subgroup are:
- Crandallite, CaAl3(PO4)2(OH)5·H2O, where calcium replaces lead
- Goyazite, SrAl3(PO4)(OH)5·H2O, where strontium replaces lead
- Philipsbornite, PbAl3(AsO4)2(OH)5·H2O, where the arsenate group AsO4 replaces the phosphate group PO4
Plumbogummite was discovered in 1819[1] and named in 1832[3] from the Latin "plumbum" for lead, and "gummi" for gum, in allusion to its lead content and appearance, which at times resembles coatings of gum.
Unit cell
Plumbogummite crystallizes in space group R3m. The reported lattice parameters (the lengths of the sides of the unit cell) vary in detail according to the source, but all agree that normal plumbogummite has "a" close to 7 Å and "c" close to 17 Å, with Z=3. Various reported values of "a" and "c"are:
- a = 7.01 Å,[1] 7.017 Å,[4] 7.018 Å,[2] 7.033 Å[3]
- c = 16.71Å,[1] 16.75 Å,[4] 16.784 Å,[2] 16.789 Å[3]
Mills et al.[5] investigated a gallium-rich sample of plumbogummite from Tsumeb, Namibia, and found larger cell parameters, with a = 7.0752 Å and c = 16.818 Å.
Structure
The basic structural units of plumbogummite are PO4 tetrahedra, with phosphorus atoms (P) at the center and oxygen atoms (O) at the corners, together with AlO6 octahedra, aluminium atoms (Al) at the center and oxygen atoms at the corners. The tetrahedra and octahedra combine by sharing corners, to form composite layers. Lead atoms (Pb) occupy sites between the layers.[5]
Environment
Plumbogummite is found in the oxidized zones of lead-bearing deposits. It commonly occurs as botryoidal, kidney shaped, stalactitic or globular crusts or masses, frequently with a concentric structure; rare crystals have a hexagonal outline. Pyromorphite and baryte are common associated minerals, and plumbogummite may be pseudomorphic after them. Other associated minerals include mimetite, duftite, cerussite, anglesite and wulfenite.[4]
Occurrence
The type locality is Huelgoat, Finistère, Brittany, France, and the type material is stored in the Natural History Museum, Paris, France.[4]
Plumbogummite has been found in the Central Cobar Mines, New South Wales, Australia[6] and the Nifty Copper Mine, Western Australia.[7] Also in the Kintore open cut at Broken Hill, New South Wales, Australia, but it is generally inconspicuous there and only a few specimens have been collected.[8]
Material from the Siglio XX Mine, Llallagua, Bolivia, is an unusual pale yellow color, rather than the more common blue or green, forming crusts on quartz and cassiterite, and enclosing crude octahedral jeanbandyite crystals with orange colored shells of plumbogummite.[9]
References
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Wikimedia Commons has media related to Plumbogummite. |
- 1 2 3 4 5 6 Mindat.org
- 1 2 3 4 Webmineral data
- 1 2 3 4 5 6 7 Gaines et al (1997) Dana's New Mineralogy Eighth Edition, Wiley
- 1 2 3 4 5 6 7 8 9 Handbook of Mineralogy
- 1 2 3 4 Mineralogical Magazine (2009) 73(5), 837–845
- ↑ Australian Journal of Mineralogy 11-2, 77
- ↑ Australian Journal of Mineralogy 12-1, 28
- ↑ Australian Journal of Mineralogy 3-1, 32 and 50
- ↑ Mineralogical Record 37-2, 127 and 148