Sylvite: Difference between revisions
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|Crystal_Structure = | |Crystal_Structure = | ||
|Deliqueszenzhumidity =85.0% | |Deliqueszenzhumidity =85.0% | ||
|Solubility = | |Solubility = 4.595 mol/kg | ||
|Density =1.987 g/cm<sup>3</sup> | |Density =1.987 g/cm<sup>3</sup> | ||
|MolVolume =37.52 cm<sup>3</sup>/mol | |MolVolume =37.52 cm<sup>3</sup>/mol | ||
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|chemBehavior = | |chemBehavior = | ||
|Comments = | |Comments = | ||
|Literature = <bib id="Robie.etal:1978"/> <bib id="Dana:1951"/> | |Literature = <bib id="Steiger.etal:2014"/> <bib id="Robie.etal:1978"/> <bib id="Dana:1951"/> | ||
}} | }} | ||
back to [[Chloride]] | back to [[Chloride]] | ||
==Solubility== | |||
[[Image:S KCl e.jpg|800px|thumb|left|'''Figure 1''': Solubility of potassium chloride in water. The molality ''m'' [n(KCl)•kg(H<sub>2</sub>O)<sup>-1</sup>] is plotted versus the temperature. According to <bib id="Steiger.etal:2008c"/>]] | |||
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==Hygroscopicity== | ==Hygroscopicity== | ||
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[[Image:D KCl e.jpg|800px|thumb|left|'''Figure 2''': Deliquescence behaviour of potassium chloride. The water activity ''a<sub>w</sub>'' is plotted versus the temperature. According to <bib id="Steiger.etal:2008c"/>]] | |||
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Latest revision as of 13:50, 17 March 2015
Sylvite[1][2] | |
Mineralogical name | Sylvite, Hövelite |
Chemical name | Potassium chloride |
Trivial name | |
Chemical formula | KCl |
Other forms | |
Crystal system | cubic |
Crystal structure | |
Deliquescence humidity 20°C | 85.0% |
Solubility (g/l) at 20°C | 4.595 mol/kg |
Density (g/cm³) | 1.987 g/cm3 |
Molar volume | 37.52 cm3/mol |
Molar weight | 74.56 g/mol |
Transparency | transparent to translucent |
Cleavage | perfect |
Crystal habit | |
Twinning | |
Phase transition | |
Chemical behavior | |
Comments | |
Crystal Optics | |
Refractive Indices | n=1.4903 |
Birefringence | |
Optical Orientation | isotropic |
Pleochroism | |
Dispersion | |
Used Literature | |
[Steiger.etal:2014]Title: Weathering and Deterioration Author: Steiger, Michael; Charola A. Elena; Sterflinger, Katja [Robie.etal:1978]Title: Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar pressure and higher temperatures Author: Robie R.A., Hemingway B.S.; Fisher J.A. [Dana:1951]Title: Dana's System of Mineralogy Author: Dana J.D. |
back to Chloride
Solubility[edit]
Hygroscopicity[edit]
0°C | 10°C | 20°C | 30°C | 40°C | 50°C |
88.3%r.h. | 86.7%r.h. | 85.0%r.h. | 83.5%r.h. | 82.1%r.h. | 80.7%r.h. |
Weblinks[edit]
- ↑ http://webmineral.com/data/Sylvite.shtml viewed on 29/07/2010
- ↑ http://www.mindat.org/min-3850.html viewed on 29/07/2010
Literature[edit]
[Dana:1951] | Dana E.S. (eds.) Dana J.D. (1951): Dana's System of Mineralogy, 7, Wiley & Sons | |
[Robie.etal:1978] | Robie R.A., Hemingway B.S.; Fisher J.A. (1978): Thermodynamic properties of minerals and related substances at 298.15 K and 1 bar pressure and higher temperatures. In: U.S. Geol. Surv. Bull, 1452 () | |
[Steiger.etal:2008c] | Steiger, Michael; Kiekbusch, Jana; Nicolai, Andreas (2008): An improved model incorporating Pitzer’s equations for calculation of thermodynamic properties of pore solutions implemented into an efficient program code. In: Construction and Building Materials, 22 (8), 1841-1850, 10.1016/j.conbuildmat.2007.04.020 | |
[Steiger.etal:2014] | Steiger, Michael; Charola A. Elena; Sterflinger, Katja (2014): Weathering and Deterioration. In: Siegesmund S.; Snethlage R. (eds.): Stone in Architecture, Springer Verlag Berlin Heidelberg, 223-316, 10.1007/978-3-642-45155-3_4. |