Shigaite | |
---|---|
![]() Reddish-brown shigaite crystal (2 cm across) with pink
rhodochrosite from South Africa | |
General | |
Category | Sulfate mineral |
Formula (repeating unit) | NaAl3(Mn2+)6(SO4)2(OH)18·12H2O [1] |
IMA symbol | Sga [2] |
Strunz classification | 7.DD.35 [3] |
Dana classification | 31.1.2.1 [3] |
Crystal system | Trigonal |
Crystal class | Rhombohedral (3) H-M symbol: (3) [3] |
Space group | R3 [4] |
Unit cell | a = 9.51 Å, c = 32.83 Å, [3] Z = 3 [5] |
Identification | |
Color | Yellow, burnt orange, brown, black [5] |
Twinning | On {0001} [5] |
Cleavage | Perfect on {0001} [5] |
Tenacity | Moderately flexible [5] |
Mohs scale hardness | 2 [5] |
Luster | Vitreous to dull [3] |
Streak | Very pale yellow to white [5] |
Diaphaneity | Transparent [3] |
Specific gravity | 2.32 [4] |
Optical properties | Uniaxial (−) [3] |
Refractive index | n = 1.546 [4] |
Pleochroism | Distinct; O = yellow; E = very pale yellow [5] |
Ultraviolet fluorescence | Non-fluorescent [4] |
Shigaite is a mineral with formula NaAl3(Mn2+)6(SO4)2(OH)18·12H2O that typically occurs as small, hexagonal crystals or thin coatings. It is named for Shiga Prefecture, Japan, where it was discovered in 1985. [3] The formula was significantly revised in 1996, identifying sodium as a previously unknown constituent.
Shigaite occurs as hexagonal tabular crystals up to 2 cm (0.79 in) in size or as thin films and coatings. The mineral can be yellow, burnt orange, brown or black in color. [5] Shigaite occurs in metamorphosed deposits of manganese ore [5] and is the Mn2+ analogue of motukoreaite. [6]
Shigaite consists of oxycation sheets of [AlMn2+2(OH)61+ intercalated with oxyanion sheets of [Na(H2O)6{H2O}6(SO4)23−. Linkage between the sheets and within the oxyanion sheet results largely through hydrogen bonding. [6]
Shigaite was discovered in 1985 in the Ioi Mine, [a] Shiga Prefecture, Japan. [3] The original study, published in the journal Neues Jahrbuch für Mineralogie, Monatshefte, [1] identified the formula as Al4Mn7(SO4)2(OH)22·8H2O. [7] The formula was significantly revised in 1996 using a sample from the N'Chwaning Mine, South Africa. [6] Sodium, discovered to be a component of shigaite, was not identified in the original study. However, an unidentified volatile had been noted that presumably was a sodium-containing complex. [8]
As of 2012 [update], shigaite is known from the following sites: [3]
The type material is housed in the National Museum of Natural History in Washington, D.C. as sample 122089. [5]
Shigaite has been found associated with the following minerals: [5]
Ioi mine, Japan
|
Wessels Mine, South Africa
|
Iron Monarch, South Australia
|
Shigaite | |
---|---|
![]() Reddish-brown shigaite crystal (2 cm across) with pink
rhodochrosite from South Africa | |
General | |
Category | Sulfate mineral |
Formula (repeating unit) | NaAl3(Mn2+)6(SO4)2(OH)18·12H2O [1] |
IMA symbol | Sga [2] |
Strunz classification | 7.DD.35 [3] |
Dana classification | 31.1.2.1 [3] |
Crystal system | Trigonal |
Crystal class | Rhombohedral (3) H-M symbol: (3) [3] |
Space group | R3 [4] |
Unit cell | a = 9.51 Å, c = 32.83 Å, [3] Z = 3 [5] |
Identification | |
Color | Yellow, burnt orange, brown, black [5] |
Twinning | On {0001} [5] |
Cleavage | Perfect on {0001} [5] |
Tenacity | Moderately flexible [5] |
Mohs scale hardness | 2 [5] |
Luster | Vitreous to dull [3] |
Streak | Very pale yellow to white [5] |
Diaphaneity | Transparent [3] |
Specific gravity | 2.32 [4] |
Optical properties | Uniaxial (−) [3] |
Refractive index | n = 1.546 [4] |
Pleochroism | Distinct; O = yellow; E = very pale yellow [5] |
Ultraviolet fluorescence | Non-fluorescent [4] |
Shigaite is a mineral with formula NaAl3(Mn2+)6(SO4)2(OH)18·12H2O that typically occurs as small, hexagonal crystals or thin coatings. It is named for Shiga Prefecture, Japan, where it was discovered in 1985. [3] The formula was significantly revised in 1996, identifying sodium as a previously unknown constituent.
Shigaite occurs as hexagonal tabular crystals up to 2 cm (0.79 in) in size or as thin films and coatings. The mineral can be yellow, burnt orange, brown or black in color. [5] Shigaite occurs in metamorphosed deposits of manganese ore [5] and is the Mn2+ analogue of motukoreaite. [6]
Shigaite consists of oxycation sheets of [AlMn2+2(OH)61+ intercalated with oxyanion sheets of [Na(H2O)6{H2O}6(SO4)23−. Linkage between the sheets and within the oxyanion sheet results largely through hydrogen bonding. [6]
Shigaite was discovered in 1985 in the Ioi Mine, [a] Shiga Prefecture, Japan. [3] The original study, published in the journal Neues Jahrbuch für Mineralogie, Monatshefte, [1] identified the formula as Al4Mn7(SO4)2(OH)22·8H2O. [7] The formula was significantly revised in 1996 using a sample from the N'Chwaning Mine, South Africa. [6] Sodium, discovered to be a component of shigaite, was not identified in the original study. However, an unidentified volatile had been noted that presumably was a sodium-containing complex. [8]
As of 2012 [update], shigaite is known from the following sites: [3]
The type material is housed in the National Museum of Natural History in Washington, D.C. as sample 122089. [5]
Shigaite has been found associated with the following minerals: [5]
Ioi mine, Japan
|
Wessels Mine, South Africa
|
Iron Monarch, South Australia
|