Santabarbaraite | |
---|---|
General | |
Category | Phosphate minerals |
Formula (repeating unit) | Fe3+3(PO4)2(OH)3·5H2O |
IMA symbol | Sbb[1] |
Strunz classification | 8.CE.80 |
Crystal system | Amorphous |
Identification | |
Color | Brown to light brown |
Crystal habit | Elongated or flattened prisms |
Twinning | None |
Cleavage | None, parting along {010} of replaced phase |
Fracture | Conchoidal |
Mohs scale hardness | Not determined |
Luster | Vitreous to greasy |
Streak | yellow-umber |
Diaphaneity | Translucent |
Specific gravity | 2.24 |
Optical properties | isotropic |
Refractive index | n = 1.659 |
Other characteristics | Pseudomorphism |
References | [2][3] |
Santabarbaraite is an amorphous ferric hydroxy phosphate mineral hydrate that was discovered in Tuscany, Italy during 2000.[4] It also can be found in Victoria, Australia and Lake Baikal, Siberia.[5]
This phosphate mineral has a simplified formula Fe3+3(PO4)2(OH)3·5H2O,[4] which is the same formula of another non-amorphous phosphate mineral called allanpringite.[6] Santabarbaraite occurs as pseudomorphic masses after vivianite (Fe2+3(PO4)2·8H2O). In the process, monoclinic vivianite oxidizes to form the amorphous santabarbaraite.[4] Pseudomorphism may be seen in Victoria, Australia, in Wannon Falls (originally a well-known locality for vivianite). It also may be seen at Lake Baikal, Siberia where the oxidized santabarbaraite may be seen as a rim surrounding vivianite due to exposure to air.[5]