Magnesium sulfate: Difference between revisions
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On objects, crystallized magnesium sulfate can appear in differing morphologies, but specific forms appear more frequently. One examined object displayed a loose crust of an opaque, gray to yellow substance in situ, which was a mixture of epsomite and hexahydrite (part of the thesis by Mainusch <bib id= "Mainusch:2001"/>). At the monastery church St. Johann at Müstair epsomite appeared as “granular crusts”. Magnesium sulfate efflorescence in the shape of salt whiskers was detected at St. Georgs church in Steiermark (Styria). | On objects, crystallized magnesium sulfate can appear in differing morphologies, but specific forms appear more frequently. One examined object displayed a loose crust of an opaque, gray to yellow substance in situ, which was a mixture of epsomite and hexahydrite (part of the thesis by Mainusch <bib id= "Mainusch:2001"/>). At the monastery church St. Johann at Müstair epsomite appeared as “granular crusts”. Magnesium sulfate efflorescence in the shape of salt whiskers was detected at St. Georgs church in Steiermark (Styria). | ||
=== Micro- chemistry === | === Micro- chemistry === | ||
=== Microscopy === | === Microscopy === | ||
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<br> | <br> | ||
== X- Ray diffraction == | == X- Ray diffraction == | ||
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= <br>Umgang mit Epsomitschäden = | = <br>Umgang mit Epsomitschäden = | ||
== Salts and deterioration pattern == | == Salts and deterioration pattern == | ||
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</gallery> | </gallery> | ||
== Unter dem Rasterelektronenmikroskop == | == Unter dem Rasterelektronenmikroskop == | ||
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Revision as of 15:56, 23 March 2015
Author: Amelie Stahlbuhk
back to Sulfate
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Abstract[edit]
The different hydrated forms of magnesium sulfate and the behaviour concerning solubility and hygroscopicity will be presented.
Hydrated forms[edit]
Kieserite MgSO4•H2O
Sanderite MgSO4•2H2O
Starkeyite MgSO4•4H2O
Pentahydrite MgSO4•5H2O
Hexahydrite MgSO4•6H2O
Epsomite MgSO4•7H2O
Meridianiite MgSO4•11H2O
Solubility[edit]
As it is shown in table 1, the different hydrated forms of magnesium sulfate are easily soluble salts, which leads to a high mobility of the salts in porous materials.
Hydrated form | Solubility [mol/kg] at 20°C |
Kieserite | 5.60 |
Starkeyite | 5.04 |
Pentahydrite | 4.40 |
Hexahydrite | 3.61 |
Epsomite | 2.84 |
Due to the different hydrated forms of magnesium sulfate with stable and meta stable equilibria, the solubility diagram of the system MgSO4-H2O contains more information than diagrams of salts with less or also without any hydrated forms. With the temperature dependence of the solubility it is possible that temperature changes are accompanied by a hydration or a dehydration of a considered phase.
Hygroscopicity[edit]
In the system MgSO4-H2O changes in temperature or relative humidity may lead to hydration/dehydration or deliquescence/crystallization processes. At 20 °C epsomite is the present crystalline phase when the relative humidity is below its deliquescence humidity of 91.3 %. When the relative humidity reaches values below 47 % the dehydration to lower hydrated levels sets in, as it is represented by the curves of the equilibrium humidities in figure 2.
Phase transition | Deliquescence or equilibrium humidity at 20°C |
Epsomite-solution | 91.3 % |
Epsomite-Hexahydrite | 46.6 % |
Epsomite-Kieserite | 46.7 % |
Hexahydrite-Starkeyite | 39.1 % |
In the temperature range of -10 to 100 °C the deliquescence humidities of the present hydrated forms (depending on the temperature) lie always above 80 % r.h., so the salts do not belong to the hygroscopic salts.
Weblinks[edit]
Literature[edit]
[Mainusch:2001] | Mainusch, Nils (2001): Erstellung einer Materialsammlung zur qualitativen Bestimmung bauschädlicher Salze für Fachleute der Restaurierung, Diplomarbeit, HAWK Hochschule für angewandte Wissenschaft und Kunst Hildesheim/Holzminden/Göttingen, file:Diplomarbeit Nils Mainusch.pdf | |
[Stark.etal:1996] | Stark, Jochen; Stürmer, Sylvia (1996): Bauschädliche Salze, Bauhaus-Univ. Weimar | |
[Steiger.etal:2011a] | Steiger, Michael; Linnow, Kirsten; Ehrhardt, Dorothee; Rohde, Mandy (2011): Decomposition reactions of magnesium sulfate hydrates and phase equilibria in the MgSO4-H2O and Na+-Mg2+-Cl--SO42--H2O systems with implications for Mars. In: Geochimica et Cosmochimica Act, 75 (12), 3600-3626, 10.1016/j.gca.2011.03.038, |