Jun 3 2014
Wardite is a hydrous sodium aluminum phosphate hydroxide mineral, and it crystallizes in the tetragonal trapezohedral class.
It was named after Henry Augustus Ward, an American collector and dealer in natural history objects from Rochester in New York, USA.
Properties of Wardite
The following are the key properties of Wardite:
- Cell Data
- Space Group: P41212 or P43212
- a = 7.03(1)
- c = 19.04(1)
- Z = 4
- Crystal Data
- Tetragonal
- Point Group: 422
- Dipyramidal pseudo-octahedral crystals, with {010}, {011}, {012}, {100}, rarely {001}, typically striated ⊥ [001], to 4cm
- X-ray powder pattern: 4.74 (10), 2.994 (7), 2.591 (7), 3.085 (6), 1.516 (5), 2.825 (4), 2.108 (4)
- Chemical Composition
Elements |
Content 1 |
Content 2 |
Al2O3 |
38.70 |
38.43 |
P2O5 |
35.12 |
35.67 |
H2O |
17.88 |
18.11 |
Na2O |
7.51 |
7.79 |
FeO |
0.26 |
|
MgO |
0.21 |
|
K2O |
0.16 |
|
Total |
99.84 |
100.00 |
- Optical Properties
- Transparent to opaque
- Color: White, colorless, pale green, blue-green, yellow-green, pale yellow, brown; colorless in transmitted light
- Luster: Vitreous
- Optical Class: Uniaxial (+)
- ω = 1.586–1.594
- ε = 1.595–1.604
- Estimated Properties
Electron density |
Bulk density (electron density) = 2.79 g/cm3
note: Specific gravity of Wardite = 2.78 g/cm3 |
Photoelectric |
PEWardite = 1.47 barns/electron
U = PEWardite x ρElectron density = 4.10 barns/cm3 |
Fermion index |
Fermion index = 0.00027
Boson index = 0.99972 |
Radioactivity
|
Wardite is not radioactive
|
How to Identify Wardite
Wardite varies from vitreous green, bluish-green, white to colorless crystal masses. It has a transparent to translucent appearance, and forms fibrous encrustations. Its radial crystals radiate from the center without producing stellar forms. It has a perfect cleavage with white streak, non-magnetic, and non-fluorescent properties.
It has a relative hardness of 5, and an average density of 2.84 g/cm3.
Global Distribution
Wardite is distributed in the following places:
- Little Green Monster mine, Clay Canyon, USA
- Dunton quarry and the Bell Pit, Newry
- Palermo #1 mine, North Groton
- Grafton Co. New Hampshire
- Hugo pegmatite, near Keystone
- Tip Top mine, 8.5km south-west of Custer, Custer Co. South Dakota
- Big Fish River–Rapid Creek area, Yukon Territory, Canada
- Lavra da Ilha pegmatite, in the Jequitinhonha River, Brazil
- Pirineus mine, Itinga, Minas Gerais
- Alto Patrimonio, Piedras Lavradas, Para´iba
- Songo, Sierra Leone
- Wolfsberg quarry, near Spittal, Carinthia, Austria
- Ruffiac, Morbihan, and Montebras, Creuse, France
- Iron Monarch quarry, Iron Knob, South Australia
- Milgun Station, Western Australia
Occurrence of Wardite and Useful Mineral Association
Wardite occurs as a component of low-temperature phosphatic nodules, and is an uncommon species in complex zoned pegmatites.
It is commonly associated with siderite roscherite (pegmatites), eosphorite, hydroxyl-herderite, fairfieldite, montgomeryite, whitlockite, mitridatite, ferrisicklerite, crandallite, millisite, and variscite.
References