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Sulfate mineral From Wikipedia, the free encyclopedia
Epsomite, Epsom salt, or magnesium sulfate heptahydrate, is a hydrous magnesium sulfate mineral with formula MgSO4·7H2O.
| Epsomite | |
|---|---|
| |
| General | |
| Category | Sulfate mineral |
| Formula (repeating unit) | MgSO4·7H2O |
| IMA symbol | Esm[1] |
| Strunz classification | 7.CB.40 |
| Dana classification | 29.6.11.1 |
| Crystal system | Orthorhombic |
| Crystal class | Disphenoidal (222) H-M symbol: (2 2 2) |
| Space group | P2₁2₁2₁ |
| Unit cell | a = 11.86, b = 11.99 c = 6.858 [Å]; Z = 4 |
| Identification | |
| Color | White, grey, colorless, or pink, greenish |
| Crystal habit | Acicular to fibrous encrustations |
| Twinning | Rarely observed on {110} |
| Cleavage | {010} perfect {101} distinct |
| Fracture | Conchoidal |
| Mohs scale hardness | 2 |
| Luster | Vitreous, silky when fibrous |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 1.67–1.68 |
| Optical properties | Biaxial (−) |
| Refractive index | nα = 1.433 nβ = 1.455 nγ = 1.461 |
| Birefringence | δ = 0.028 |
| 2V angle | Measured: 52° |
| Solubility | In water |
| Alters to | Dehydrates in dry air |
| References | [2][3][4] |
Epsomite crystallizes in the orthorhombic system. The normal form is as massive encrustations, while acicular or fibrous crystals are rarely found. It is colorless to white with tints of yellow, green and pink. It is a soft mineral with variable Mohs hardness around 2.0~2.5, and it has a low specific gravity of 1.67.[5]
It is readily soluble in water, and absorbs water from the air. It converts to hexahydrate with the loss of one water molecule and a switch to monoclinic structure.[5]
The epsomite group includes solid solution series with morenosite (NiSO
4·7 H
2O) and goslarite (ZnSO
4·7 H
2O).[3][clarification needed]
It was first systematically described in 1806 for an occurrence near Epsom, Surrey, England, after which it was named.[5] It has been also referred to as "cave cotton" when in its fibrous form.[6]
Epsomite forms as encrustations or efflorescences on limestone cavern walls and mine timbers and walls, rarely as volcanic fumarole deposits, and as rare beds in evaporite layers such as those found in certain bodies of salt water.[5][7] It occurs in association with melanterite, gypsum, halotrichite, pickeringite, alunogen, rozenite, and mirabilite.[4]
Naturally occurring epsomite in caverns can potentially produce particulates of inhalable size, and may contain significant amounts of toxic impurities.[6][8]
Epsom salt is commonly sold as the main ingredient in bath salt, with additives such as glycerin (used as a humectant) and fragrances. The purpose of bath salts is mostly to make the bathing experience more enjoyable and serve as a vehicle for cosmetics, though they are said to improve cleaning and aid in exfoliation.[9]
Research on topical magnesium (for example Epsom salt baths) is very limited.[10] The trade organization 'Epsom Salt Council' recommends bathing 2 or 3 times/week, using 500–600 g (18–21 oz) Epsom salts each time.[11]
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