Salammoniac | |
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General | |
Category | Halide mineral |
Formula (repeating unit) | NH4Cl |
IMA symbol | Sam[1] |
Strunz classification | 3.AA.25 |
Crystal system | Isometric |
Crystal class | Hexoctahedral (m3m) H-M symbol: (4/m 3 2/m) |
Space group | Pm3m |
Unit cell | a = 3.859 Å; Z = 1 |
Identification | |
Formula mass | 53.49 g/mol |
Color | Colorless, white, pale gray; may be pale yellow to brown, if impure. |
Crystal habit | Crystals skeletal or dendritic; massive, encrustations |
Twinning | On {111} |
Cleavage | Imperfect on {111} |
Fracture | Conchoidal |
Tenacity | Sectile |
Mohs scale hardness | 1–2 |
Luster | Vitreous |
Streak | White |
Diaphaneity | Transparent |
Specific gravity | 1.535 |
Optical properties | Isotropic |
Refractive index | n = 1.639 |
Birefringence | Weak after deformation |
Ultraviolet fluorescence | No |
Absorption spectra | No |
Solubility | In water |
References | [2][3][4] |
Salammoniac,[2] also sal ammoniac or salmiac, is a rare naturally occurring mineral composed of ammonium chloride, NH4Cl. It forms colorless, white, or yellow-brown crystals in the isometric-hexoctahedral class. It has very poor cleavage and is brittle to conchoidal fracture. It is quite soft, with a Mohs hardness of 1.5 to 2, and it has a low specific gravity of 1.5. It is water-soluble. Salammoniac is also the archaic name for the chemical compound ammonium chloride.