Epsomite
| 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 g/ml |
| 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, Epsom salt, or magnesium sulfate heptahydrate, is a hydrous magnesium sulfate mineral with formula MgSO4·7H2O.
Physical properties
Epsomite crystallizes in the orthorhombic system. The normal form is as massive encrustations, while acicular or fibrous crystals are as 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 g/ml.
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.
The epsomite group includes solid solution series with morenosite (NiSO
4·7 H
2O) and goslarite (ZnSO
4·7 H
2O).[3][clarification needed]
Etymology
It was first systematically described in 1806 for an occurrence near Epsom, Surrey, England, after which it was named.
Occurrence
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] It occurs in association with melanterite, gypsum, halotrichite, pickeringite, alunogen, rozenite, and mirabilite.[4]
Uses
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.[6]
Research on topical magnesium (for example Epsom salt baths) is very limited.[7] The trade organization 'Epsom Salt Council' recommends bathing 2 or 3 times/week, using 500–600 g (18–21 oz) Epsom salts each time.[8]
See also
References
- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. Vol. 85, no. 3. pp. 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ "Epsomite". Web Mineral (webmineral.com).
- ^ a b "Epsomite". Mindat.org.
- ^ a b Epsomite (PDF) (Report). Handbook of Mineralogy – via Dept. Geology, University of Arizona.
- ^ McGraw-Hill Encyclopedia of Science & Technology (10th ed.). New York, NY: McGraw-Hill. 2007. ISBN 9780071441438. OCLC 84152915.
- ^ Browning, Marie (1999). Natural Soapmaking (1st ppb ed.). New York, NY: Sterling. ISBN 0-8069-6289-5. OCLC 42598586.
- ^ Rath, Linda. "Why take an epsom salts bath?". WebMD (webmd.com). A-to-Z guides.
- ^ Report on absorption of magnesium sulfate (PDF) (commercial / promotional). Epsom Salt Council. October 2015 – via epsomsaltcouncil.org.
- "Epsomite". Sulfates. Mineral galleries (mineral.galleries.com). Archived from the original on 17 March 2006.
