Talk:Gypsum: Difference between revisions

From Saltwiki
Jump to navigation Jump to search
No edit summary
(Replaced content with "text copied to the content page ~~~~ SLeithaeuser 15:42, 22 January 2012 (CET) Still in progress")
 
Line 1: Line 1:
http://193.175.110.91/saltwiki/index.php/Talk:Welcome_to_SaltWiki
text copied to the content page [[User:Hschwarz|Hschwarz]] 13:42, 24 January 2012 (CET)
 
<bibimport/>
{{Infobox_Salt
|Footnote            = <ref>http://webmineral.com/data/Gypsum.shtml seen on 30.07.2010</ref><ref>http://www.mindat.org/min-1784.html seen on 30.07.2010</ref>
|photo                = [[File:SA101 1.jpeg|300px]]
|mineralogical_Name  = Gypsum, Selenite
|chemical_Name        = Calcium sulfate dihydrate
|Trivial_Name        = Gypsum, plaster of paris
|chemical_Formula    = Ca[SO<sub>4</sub>]•2H<sub>2</sub>O
|Hydratforms          = Anhydrite (CaSO<sub>4</sub>)<br>Hemihydrate (CaSO<sub>4</sub>•0.5H<sub>2</sub>O)
|Crystal_System      = monoclinic
|Crystal_Structure    =
|Deliqueszenzhumidity =
|Solubility          = 2.14 g/l
|Density              = 2.2-2.4 g/cm³
|MolVolume            = 74.69 cm<sup>3</sup>/mol
|Molweight            = 172.17g /mol
|Transparency        = transparent to opaque
|Cleavage            = perfect, clearly visible formation of fibre
|Crystal_Habit        =  flat, prismatic, needle- like crystal,  granular, massive aggregate
|Twinning            = very common
|Refractive_Indices  = α = 1.519-1.521<br>β = 1.522-1.523<br>γ = 1.529-1.530
|Birefringence        = Δ = 0.010
|optical_Orientation  = biaxial positive
|Pleochroism          = colorless
|Dispersion          = 58°
|Phase_Transition    =
|chemBehavior        = hardly soluble in water
|Comments            =
}}
Authors:  [[user:Hschwarz|Hans-Jürgen Schwarz ]], Nils Mainusch, [[user:TMueller|Tim Müller]]
<br>back to [[Sulfate]]
 
=Calciumsulfate and Gipsum =
 
== Abstract  ==
 
This article deals with the system CaSO<sub>4</sub>/H<sub>2</sub>O, in particular with gypsum. Gypsum is one of the most important salts responsible for the damage on buildings and wallpaintings. Especially objects exposed to exterior conditions are prone to damage from gypsum. The properties, the effect of the damage, the appearance, but also examination methods are included in the following article. Images, micro photos and examples from practical experiences illustrate the subject.<br>
<br>
 
== Introduction  ==
 
Gypsum is one of the most common salts causing the deterioration of constructions. It is present in very different types and characteristics, nearly on all external constructions, but can also to be found in the internal environment. <br>
<br>
<br>
 
== Occurrence of Gypsum  ==
 
One of the most prevalent minerals, gypsum forms by precipitation from aqueous solution at temperatures under approximately 40°C. At increased temperatures (&gt; 60°C) of a solution the formation of anhydrite takes place directly. Calcium sulfate and calcium sulfate dihydrate are often present in rocks. Hemihydrate does not occur naturally.<br>
Gypsum occurs naturally in salt deposits and salt deserts, where sometimes desert rose crystals form in combination with quartz inclusions. In salt deposits gypsum and anhydrite sometimes form a caprock, i.e. a massive layer of material covering a natural salt deposit.
Synthetic gypsum is produced in coal-fired power plants, as a by-product of  flue- gas desulferization. 
 
== Origin and formation of gypsum on monuments ==
 
The relevance of the damage caused by gypsum, on monuments made from mineral building materials, is substantially linked to the conversion reaction from lime to gypsum. When exposed to air containing SO<sub>x</sub> and in combination with moisture, important material components of buildings can be converted into gypsum. The reaction takes place as follows: 
 
CaCO<sub>3</sub> + H<sub>2</sub>SO<sub>4</sub> → CaSO<sub>4</sub> + H<sub>2</sub>O + CO<sub>2</sub>
 
Moreover, gypsum as a major component of mortars, plasters and some building stones (e.g. anhydrite) can be an original building material, an integral part of the monuments fabric.
<br>
<br>
<br>
 
==  Damage potential and weathering activity  ==
 
=== Solubility properties  ===
 
[[file:CaSO4 sol.JPG|thumb|350px|left|'''Figure1:''' Solubility of CaSO4 in water (diagram: Michael Steiger)]]
<br>Gypsum belongs to the group of salts with a low solubility in aqueous solution and therefore it can be described as less mobile than others. However, the influence of ions from other sources is comparatively high. For example, the presence of halite can increase the solubility of gypsum in dependence of the concentration ratio, up to the factor of four.  <br>
 
[[file:Loeslichkeit Gips 02.JPG|thumb|left|350px|'''Figure 2:'''Solubility of gypsum compared with other salts  (after <bib id=Stark.etal:1996/>)]]
<br clear=all>
 
=== Hydration behavior  ===
 
The system CaSO<sub>4 </sub>– H<sub>2</sub>O: <br> calcium sulfate can appear in three different hydrate phases:
*anhydrite- the above mentioned anhydrous form
*hemihydrate- the least stable form
*Gypsum- calcium sulfate dihydrate 
Anhydrite exists in different modifications, resulting in different chemical properties, in dependence of the modification (e.g. varying solubility in water). The same applies for hemihydrate. <br>
A value for the transition temperature (in aqueous solution) is the range of between 40°C-66°C. Under normal climatic conditions, on  monuments, the precipitation of calcium sulfate from aqueous solution will therefore be predominantly gypsum. Anhydrite forms when the temperature in solution is higher than 40°C-60°C. Parallel to this the formation of large amounts of the metastable hemihydrate takes place during precipitation, it is later transformed into more stable hydrate phases. <br>
When heating the dihydrate (as a solid and dry) to approximately 50°C,  the chemically combined water is expelled and hemihydrate forms. However, a complete transition to hemihydrate only takes place at temperatures of around 100°C. If dihydrate is heated to 500-600°C, the anhydrous calcium sulfate is formed. At temperatures above 1000°C the thermal decomposition into calcium oxide and SO<sub>3</sub> is effected.
<br clear=all>
 
 
=== Hygroscopicity ===
 
[[File:Veraenderung Loeslichkeit durch Fremdionen Gips .JPG|thumb|right|350px|'''Figure 3''':
The modification of the solubility of gypsum in water, in the presence of [[halite]], is shown in Figure 3. If the concentration of halite is approximately 140 g/l in aqueous solution, around 8 g gypsum is dissolved (Angaben nach <bib id=DAns:1933/>)]]. The pure gypsum salt has no defined [[deliquescence|Deliquescence]] point. If, in the presence of halite, relative Humidity levels exceed 90 % RH, gypsum crystals may dissolve, due to the sorption behavior of halite. A decrease of humidity levels to approximately 75% RH causes the recrystallization of gypsum.   
 
=== Crystallization pressure  ===
 
At crystallization in aqueous solution, with the saturation at a ration of 2:1, gypsum produces a linear growth pressure of 28,2-33,4 N/mm<sup>2</sup> within a temperature range of 0-50°C.  In comparison with other damaging salts, these values lie in the middle range of a calculated  scale of values reaching from 7,2 to 65,4 N/mm<sup>2</sup> [according to <bib id=Winkler:1975/>].
 
=== Hydration pressure  ===
 
Gypsum as a constituent of an object, can only release the water of crystallization (chemically combined water) at temperatures of approx.  50°C, i.e. it will normally not dehydrate. In contrast the enclosure of the water of crystallization is possible, if anhydrite or hemihydrate are present in a monument. Both processes are associated with a change in volume (of 31.9 % at the conversion from  hemihydrate- gypsum) and the emergence of [[Schadensmechanismen|Hydratationsdrücken]] [Zahlenwerte nach <bib id="Sperling.etal:1980"/>]. In the instance of a conversion from hemihydrate- gypsum (keyword Gipstreiben)  at temperatures ranging from 0-20°C and an RH or 80%, a hydration pressure of 114 –160 N/mm<sup>2</sup> can be effected- an extremely high value [ <bib id=Stark.etal:1996/>].
 
== Conversion reaction  ==
 
The hazardous character of gypsum to historic substance, is connected to the conversion reaction [[calcite]]- gypsum. The gypsum molecules formed by calcite hold a volume, that exceeds the volume of the original calcite molecule by about 100%. In this context a relevant damage factor is the modification of the water solubility. Calcite has a water solubility of approx. 0,014g/l (20°C) and is therefore more difficult to dissolve than gypsum. When a conversion to gypsum takes place the result is a more water sensitive system. N.B. The research by Snethlage and Wendler [<bib id=Snethlage.etal:1998/>] analyses the influence of gypsum on the linear hygroscopic expansion of certain sandstone materials. The damages and the change in swelling behavior of the material was explained through the influence of gypsum.
<br>
 
== Analytical identification  ==
 
 
=== Micro-chemistry ===
 
=== Microscopy  ===
 
'''Laboratory examination:''' Gypsum is slightly water soluble, therefore gypsum-containing sample material only dissolves slightly, when mixed with distilled Water.  In solution, gypsum- containing sample material recrystallizes by carefully concentrating the solvent. At first, single needles form, then increasingly needle- like gypsum aggregate in proximity of the seam of the solvent emerges. Alternatively, sample material can be dissolved in hydrochloric acid, which also leads to the formation of crystal needles. Compared to other salts that can recrystallize in needle-like shapes, e.g. [[natrite|sodium carbonate]], gypsum needles are clearly shorter.<br>
 
'''Refraction indices:''' &nbsp;&nbsp;
n<sub>x</sub> = 1.521; n<sub>y</sub> =1.523; n<sub>z</sub> =1.530<br>
 
'''birefringence''':&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; Δ = 0.009<br>'''crystal class'''e:&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; monoclinic<br>
 
'''[[Polarized light microscopy|Polarized light microscopy examination:]]'''<br>
Apart from the typical acicular habit of gypsum crystals, (especially in recrystallized material) different morphological characteristics appear. These
can be useful for identifying gypsum. Gypsum particles (in raw material samples) display shapes of rounded fragments and plate- like rhombohedra, clearly showing the inner cleavage planes. Furthermore, the occurrence of twinning shapes is typical for gypsum crystals, whether they are lath- shaped, tabular or lamellar. The assignment of refractive indices is carried out in accordance with the immersion method  using media with indices nD=1,518 und nD=1,53. Due to the often small- scale particles the examination using the Schoeder van der Kolk method is more significant and reliable than the Becke- Line test.
Gypsum crystals belong to the class of monoclinic crystals. Thus, they show, depending on the orientation of the single particle under the microscope, a parallel or respectively a symmetrical extinction, but mainly exhibit a characteristicly oblique axis position in the extinction position. On well developed crystal rhombi the oblique extinction can clearly be measured. Of all calcium sulfate crystals, gypsum has the lowest birefringence. Under crossed polarizers, gypsum has very low interference colors, lying within the gray to yellowish white range of the first order, (of course depending on the thickness of the particles).
 
<br>
'''Possibility for mistakes:'''<br>
The Analysis methods mentioned above clearly identify gypsum, provided the following evaluation criteria are explicitly clarified.<br>
 
*low water solubility
*characteristic needle- like morphology of the recrystallized particles
*all observable indices have a  n<sub>D</sub> –value from 1,518 and 1,530
*gypsum crystalslow interference colors
*gypsum crystals have an oblique extinction
 
 
{|border="2" cellspacing="0" cellpadding="4" width="60%" align="left" class="wikitable"
|+''Table 1: Salt phases with a gypsum- like chemical and optical properties''                 
|-
|bgcolor = "#F0F0F0"|'''salt phase'''
|bgcolor = "#F0F0F0"|'''differentiating factors'''
|-
|bgcolor = "#F7F7F7"|'''[[Syngenite]]''' K<sub>2</sub>Ca(SO<sub>4)</sub> • 2H<sub>2</sub>O
|bgcolor = "#FFFFEO"|all observable indices; 1,518
|-
|bgcolor = "#F7F7F7"|'''[[Tachyhydrite]]''' CaMg<sub>2</sub>Cl<sub>6</sub> • 12H<sub>2</sub>O
|bgcolor = "#FFFFEO"|mostly observable indice &lt; 1,518 / only parallel and symmetrical extinction
|-
|bgcolor = "#F7F7F7"|'''[[Hydromagnesite]]''' Mg<sub>5</sub>[OH(CO<sub>3</sub>)<sub>2</sub>]<sub>2</sub> • 4H<sub>2</sub>O
|bgcolor = "#FFFFEO"|mostly one indice &gt; 1,53
|}
<br clear="all"> <br>
 
== X- Ray diffraction  ==
 
== Raman-spectroscopy  ==
 
== DTA / TG  ==
 
== IR-spectroscopie  ==
 
= Handling of damage caused by gypsum  =
 
 
 
== Photos of gypsum crystals and deterioration pattern caused by gypsum==
 
=== On an object  ===
 
<gallery caption="" widths="200px" heights="150px" perrow="3">
Image:Perleberg 14.04.2003 (50)-Ausschnitt.jpg|Salt damage on a brick, St. Jakobi Church, Perleberg
Image:|
Image:|
</gallery>
 
<br clear=all>
=== Under the polarising microscope  ===
 
<gallery caption="In thin section of bricks" widths="200px" heights="150px" perrow="3">
 
Image:Per_270603_5-13_14.jpg|Brick with gypsum caused damage, St. Jakobi Church, Perleberg, Germany
Image:Per_270603_5-13_15.jpg|Brick with gypsum caused damage, St. Jakobi Church, Perleberg, Germany
Image:Eilsum_Gips_duennschliff.jpg|Gypsum crystals between plaster layers
 
</gallery>
 
<gallery caption="Gypsum crystallized out of a solution in water on a glass slide" widths="200px" heights="150px" perrow="3">
 
Image:CaSO4 pol 400x 01.JPG|Calcium sulfate crystallized out of a solution in water on a glass slide
Image:CaSO4+NaCl reale Probe 01.JPG|Calcium sulfate with sodium chloride of a real sample, Gypsum crystallized out of a solution in water on a glass slide
Image:CaSO4+NaCl reale Probe 02.JPG|Calcium sulfate with sodium chloride of a real sample, Gypsum crystallized out of a solution in water on a glass slide
Image:HJS CaSO4 092503-1.jpg|Calcium sulfate, Gypsum crystallized out of a solution in water on a glass slide 
</gallery>
 
<br clear=all> 
== Under the Scanning Electron Microscope (SEM)== 
<gallery caption="In a SEM" widths="200px" heights="150px" perrow="3"> 
Image:SA100_1.jpg | Gypsum crystals in a SEM
Image:SG2-2.jpeg  |  Gypsum crystals in a SEM
Image:SG2-3.jpg |  Gypsum crystals in a SEM
Image:SG3-SPC2.jpeg|EDX spektra of gypsum crystals in a SEM 
Image:SG3-3.jpeg  |  Gypsum crystals in a SEM
Image:SG3-4.jpeg | Gypsum crystals in a SEM
Image:SG1-5.jpeg | Gypsum crystals in a SEM
Image:SG1-SPC.jpeg| EDX spektra of gypsum crystals in a SEM 
</gallery>
<br clear=all>
 
==  Weblinks == 
 
<references />
 
== Literatur  == 
<bibprint/>
 
==  Weblinks == 
 
 
<references /> 
 




[[User:SLeithaeuser|SLeithaeuser]] 15:42, 22 January 2012 (CET) Still in progress
[[User:SLeithaeuser|SLeithaeuser]] 15:42, 22 January 2012 (CET) Still in progress

Latest revision as of 12:42, 24 January 2012

text copied to the content page Hschwarz 13:42, 24 January 2012 (CET)


SLeithaeuser 15:42, 22 January 2012 (CET) Still in progress

Retrieved from "https://www.saltwiki.net/index.php?title=Talk:Gypsum&oldid=3126"