Hellyerite | |
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General | |
Category | Carbonate mineral |
Formula (repeating unit) | NiCO3·5.5(H2O) |
IMA symbol | Hy[1] |
Strunz classification | 5.CA.20 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | C2/c |
Unit cell | a = 10.77, b = 7.29 c = 18.68 [Å]; β = 94°: Z = 8 |
Identification | |
Color | Pale blue |
Crystal habit | As crystal fragments and microcrystalline coatings |
Twinning | Fine lamellar parallel to cleavage |
Cleavage | One perfect, two good at 112° to each other and perpendicular to the perfect cleavage |
Mohs scale hardness | 2.5 |
Luster | Vitreous |
Diaphaneity | Semitransparent |
Specific gravity | 1.97 |
Optical properties | Biaxial (−) |
Refractive index | nα = 1.455 nβ = 1.503 nγ = 1.549 |
Birefringence | δ = 0.094 |
Pleochroism | X = Y = very pale greenish blue; Z = pale greenish blue |
2V angle | Measured: 85° |
Alters to | Decomposes on air exposure |
References | [2][3][4] |
Hellyerite, NiCO3·6(H2O), is an hydrated nickel carbonate mineral. It is light blue to bright green in colour, has a hardness of 2.5, a vitreous luster, a white streak and crystallises in the monoclinic system. The crystal habit is as platy and mammillary encrustations on its matrix. It is a pentahydrate according to X-ray crystallography. The solid consists of [Ni2(CO3)2(H2O)8] subunits with an extra pair of water of hydration.[5]