Calcium sulfate: Difference between revisions

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| verifiedrevid = 443496462
| Name = Calcium sulfate
| ImageFile1= CaSO4simple.svg
| ImageFile = CaSO4.tif
| ImageSize =
| ImageName = Calcium sulphate anhydrous
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|Section2={{Chembox Properties
| Density = 2.96 g/cm<sup>3</sup> (anhydrous) <br> 2.32 g/cm<sup>3</sup> (dihydrate)
| Solubility = 0.26 g/100ml at 25&nbsp;°C (dihydrate)<ref>{{cite journal |last1=Lebedev |first1=A. L. |last2=Kosorukov |first2=V. L. |date=2017 |title= Gypsum Solubility in Water at 25°C |url=https://link.springer.com/content/pdf/10.1134/S0016702917010062.pdf |journal=Geochemistry International |volume=55 |issue=2 |pages=171–177 |doi=10.1134/S0016702917010062|bibcode=2017GeocI..55..205L |s2cid=132916752 }}</ref>
| Solvent = [[glycerol]]
| SolubleOther = slightly soluble (dihydrate)
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==Hydration states and crystallographic structures==
[[Image:CaSO4.tif|thumb|left|Structure of the hemihydrate of calcium sulfate reveals a dense network of Ca-O-S bonds. Color code: red (O), green (Ca), orange (S).]]
The compound exists in three levels of hydration corresponding to different crystallographic structures and to minerals:
* {{chem|CaSO|4}} ([[anhydrite]]): anhydrous state.<ref>{{cite journal| doi = 10.1107/S0567740875007145| title = Anhydrite: A refinement| journal = Acta Crystallographica Section B| volume = 31| issue = 8| pages = 2164| year = 1975| last1 = Morikawa| first1 = H.| last2 = Minato| first2 = I.| last3 = Tomita| first3 = T.| last4 = Iwai| first4 = S.| bibcode = 1975AcCrB..31.2164M}}</ref> The structure is related to that of [[zirconium orthosilicate]] (zircon): {{chem|Ca||2+}} is 8-coordinate, {{chem|SO|4|2-}} is tetrahedral, O is 3-coordinate.
* {{chem|CaSO|4|·2H|2|O}} ([[gypsum]] and [[selenite (mineral)]]): dihydrate.<ref>{{cite journal| doi = 10.1107/S0567740874004055| title = A refinement of the crystal structure of gypsum {{chem|CaSO|4|·2H|2|O}}| journal = Acta Crystallographica Section B| volume = 30| issue = 4| pages = 921| year = 1974| last1 = Cole| first1 = W.F.| last2 = Lancucki| first2 = C.J.| doi-access = }}</ref>
* {{chem|CaSO|4|·{{sfrac|2}}H|2|O}} ([[bassanite]]): hemihydrate, also known as [[plaster of Paris]]. Specific hemihydrates are sometimes distinguished: α-hemihydrate and β-hemihydrate.<ref name=t>Taylor H.F.W. (1990) ''Cement Chemistry''. Academic Press, {{ISBN|0-12-683900-X}}, pp. 186-187.</ref>
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Calcium sulfate has a long history of use in dentistry.<ref>{{Cite journal|last1=Titus|first1=Harry W.|last2=McNally|first2=Edmund|last3=Hilberg|first3=Frank C.|date=1933-01-01|title=Effect of Calcium Carbonate and Calcium Sulphate on Bone Development|journal=Poultry Science|language=en|volume=12|issue=1|pages=5–8|doi=10.3382/ps.0120005|issn=0032-5791|doi-access=free}}</ref> It has been used in bone regeneration as a graft material and graft binder (or extender) and as a barrier in guided bone tissue regeneration. It is a biocompatible material and is completely resorbed following implantation.<ref>{{Cite journal |last1=Thomas |first1=Mark V. |last2=Puleo |first2=David A. |last3=Al-Sabbagh |first3=Mohanad |date=2005 |title=Calcium sulfate: a review |url=https://pubmed.ncbi.nlm.nih.gov/16393128/ |journal=Journal of Long-Term Effects of Medical Implants |volume=15 |issue=6 |pages=599–607 |doi=10.1615/jlongtermeffmedimplants.v15.i6.30 |issn=1050-6934 |pmid=16393128}}</ref> It does not evoke a significant host response and creates a calcium-rich milieu in the area of implantation.<ref>{{Cite web|date=2020-03-25|title=Biphasic Calcium Sulfate - Overview|url=https://www.augmabio.com/abca/clinical-literature/biphasic-calcium-sulfate-overview/|access-date=2020-07-16|website=Augma Biomaterials}}</ref>
 
===Other usesDesiccant===
[[File:Drierite.jpg|thumb|left|upright|150px|The desiccant Drierite|right]]
When sold at the anhydrous state as a desiccant with a color-indicating agent under the name [[Drierite]], it appears blue (anhydrous) or pink (hydrated) due to impregnation with [[cobalt(II) chloride]], which functions as a moisture indicator.
 
===Sulfuric acid production===
Up to the 1970s, commercial quantities of [[sulfuric acid]] were produced in [[Whitehaven]] ([[Cumbria]], UK) from anhydrous calcium sulfate. Upon being mixed with [[shale]] or [[marl]], and roasted, the sulfate liberates [[sulfur dioxide]] gas, a precursor in [[sulfuric acid]] production, the reaction also produces [[calcium silicate]], a mineral phase essential in [[cement]] [[Clinker (cement)|clinker]] production.<ref>[http://www.lakestay.co.uk/whitehavenmininghistory.html Whitehaven Coast Archeological Survey]</ref>
Up to the 1970s, commercial quantities of [[sulfuric acid]] were produced from anhydrous calcium sulfate.<ref>[https://www.cementkilns.co.uk/cement_kiln_whitehaven.html Whitehaven Cement Plant]</ref> Upon being mixed with [[shale]] or [[marl]], and roasted at 1400°C, the sulfate liberates [[sulfur dioxide]] gas, a precursor to [[sulfuric acid]]. The reaction also produces [[calcium silicate]], used in [[cement]] [[Clinker (cement)|clinker]] production.<ref name="anhydrite process">[https://www.cementkilns.co.uk/cemkilndoc054.html Anhydrite Process]</ref><ref>[https://d28rz98at9flks.cloudfront.net/9554/Rec1949_044.pdf COMMONWEALTH OF AUSTRALIA. DEPARTMENT OF SUPPLY AND SHIPPING. BUREAU OF MINERAL RESOURCES GEOLOGY AND GEOPHYSICS. REPORT NO.1949/44 (Geol. Ser. No. 27) by E.K. Sturmfels THE PRODUCTION OF SULPHURIC ACID AND PORTLAND CEMENT FROM CALCIUM SULPHATE AND ALUMINIUM SILICATES]</ref>
:{{chem2|2 CaSO4 + 2 SiO2 + C → 2 CaSiO3 + 2 SO2 + CO2}}
 
Some component reactions pertaining to calcium sulfate:
: 2 CaSO<sub>4</sub> + 2 SiO<sub>2</sub> → 2 CaSiO<sub>3</sub> + 2 SO<sub>2</sub> + O<sub>2</sub> <ref>[https://d28rz98at9flks.cloudfront.net/9554/Rec1949_044.pdf COMMONWEALTH OF AUSTRALIA. DEPARTMENT OF SUPPLY AND SHIPPING. BUREAU OF MINERAL RESOURCES GEOLOGY AND GEOPHYSICS. REPORT NO.1949/44 (Geol. Ser. No. 27) by E.K. Sturmfels THE PRODUCTION OF SULPHURIC ACID AND PORTLAND CEMENT FROM CALCIUM SULPHATE AND ALUMINIUM SILICATES]</ref>
:{{chem2|CaSO4 + 2 C → CaS + 2 CO2}}
 
:{{chem2|3 CaSO4 + CaS + 2 SiO2 → 2 Ca2SiO4 + 4 SO2}}
The plant made sulfuric acid by the “Anhydrite Process”, in which [[cement clinker]] itself was a by-product. In this process, anhydrite (calcium sulfate) replaces limestone in a cement rawmix, and under reducing conditions, [[sulfur dioxide]] is evolved instead of [[carbon dioxide]]. The sulfur dioxide is converted to sulfuric acid by the [[Contact Process]] using a [[vanadium pentoxide]] [[catalyst]].<ref name="Whitehaven anhydrate process">[https://www.cementkilns.co.uk/waste.html#anhydrite Whitehaven anhydrate process]</ref>
:{{chem2|3 CaSO4 + CaS → 4 CaO + 4 SO2}}
 
:{{chem2|Ca2SiO4 + CaO → Ca3OSiO4}}
CaSO<sub>4</sub> + 2 C → CaS + 2CO<sub>2</sub>
 
3 CaSO<sub>4</sub> + CaS + 2 SiO<sub>2</sub> → 2 Ca<sub>2</sub>SiO<sub>4</sub> ([[belite]]) + 4 SO<sub>2</sub>
 
3 CaSO<sub>4</sub> + CaS → 4 CaO + 4 SO<sub>2</sub>
 
Ca<sub>2</sub>SiO<sub>4</sub> + CaO → Ca<sub>3</sub>OSiO<sub>4</sub> ([[alite]])
 
2 SO<sub>2</sub> + O<sub>2</sub> → 2 SO<sub>3</sub>
(in the presence of the [[catalyst]] [[vanadium pentoxide]])
 
SO<sub>3</sub> + H<sub>2</sub>O → H<sub>2</sub>SO<sub>4</sub> <ref name="Whitehaven anhydrate process"/>
 
Because of its use in an expanding niche market, the Whitehaven plant continued to expand in a manner not shared by the other Anhydrite Process plants. The anhydrite mine opened on 11/1/1955, and the acid plant started on 14/11/1955. For a while in the early 1970s, it became the largest sulfuric acid plant in the UK, making about 13% of national production, and it was by far the largest Anhydrite Process plant ever built.<ref>[https://www.cementkilns.co.uk/cement_kiln_whitehaven.htmlInternet website cement kilns whitehaven]{{Dead link|date=November 2023 |bot=InternetArchiveBot |fix-attempted=yes }}</ref>
 
==Production and occurrence==
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In addition to natural sources, calcium sulfate is produced as a by-product in a number of processes:
*In [[flue-gas desulfurization]], exhaust gases from [[fossil-fuel power station]]s and other processes (e.g. cement manufacture) are scrubbed to reduce their sulfur oxidedioxide content, by injecting finely ground [[limestone]]:<ref>{{cite book |doi=10.1002/0471238961.0701190519160509.a01|chapter=Fuels, Synthetic, Gaseous Fuels |title=Kirk‐OthmerKirk-Othmer Encyclopedia of Chemical Technology |year=2000 |last1=Speight |first1=James G. |isbn=9780471484943 }}</ref>
:{{chem2|SO2 + 0.5 O2 + CaCO3 -> CaSO4 + CO2}}
Related sulfur-trapping methods use [[calcium hydroxide|lime]] and some produces an impure [[calcium sulfite]], which oxidizes on storage to calcium sulfate.
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Calcium sulfate is also a common component of [[fouling]] deposits in industrial heat exchangers, because its solubility decreases with increasing temperature (see the specific section on the retrograde solubility).
 
==Solubility==
==Retrograde solubility==
[[File:Temperature dependence calcium sulfate solubility.svg|thumb|400px|left|Temperature dependence of the solubility of calcium sulfate (3 phases) in pure water.]]{{clear left}}
The dissolution of the different crystalline phases of calcium sulfate in water is [[exothermic]] and releases [[heat]] (decrease in [[Enthalpy]]: ΔH < 0). As an immediate consequence, to proceed, the dissolution reaction needs to evacuate this heat that can be considered as a product of reaction. If the system is cooled, the dissolution equilibrium will evolve towards the right according to the [[Le Chatelier principle]] and calcium sulfate will dissolve more easily. Thus the solubility of calcium sulfate increases as the temperature decreases and vice versa. If the temperature of the system is raised, the reaction heat cannot dissipate and the equilibrium will regress towards the left according to Le Chatelier principle. The solubility of calcium sulfate decreases as temperature increases. This counter-intuitive solubility behaviour is called retrograde solubility. It is less common than for most of the salts whose dissolution reaction is [[endothermic]] (i.e., the reaction consumes heat: increase in [[Enthalpy]]: ΔH > 0) and whose solubility increases with temperature. Another calcium compound, [[calcium hydroxide]] (Ca(OH)<sub>2</sub>, [[portlandite]]) also exhibits a retrograde solubility for the same thermodynamic reason: because its dissolution reaction is also exothermic and releases heat. So, to dissolve the maximum amount of calcium sulfate or calcium hydroxide in water, it is necessary to cool the solution down close to its freezing point instead of increasing its temperature.
The solubility of calcium sulfate decreases as temperature increases. This behaviour ("retrograde solubility") is uncommon: dissolution of most of the salts is [[endothermic]] and their solubility increases with temperature.The retrograde solubility of calcium sulfate is also responsible for its precipitation in the hottest zone of heating systems and for its contribution to the formation of [[Fouling#Precipitation fouling|scale]] in [[boiler]]s along with the precipitation of [[calcium carbonate]] whose [[solubility]] also decreases when [[Carbon dioxide|CO<sub>2</sub>]] degasses from hot water or can escape out of the system.
 
[[File:Temperature dependence calcium sulfate solubility.svg|thumb|400px|left|Temperature dependence of the solubility of calcium sulfate (3 phases) in pure water.]]{{clear left}}
 
The retrograde solubility of calcium sulfate is also responsible for its precipitation in the hottest zone of heating systems and for its contribution to the formation of [[Fouling#Precipitation fouling|scale]] in [[boiler]]s along with the precipitation of [[calcium carbonate]] whose [[solubility]] also decreases when [[Carbon dioxide|CO<sub>2</sub>]] degasses from hot water or can escape out of the system.
 
==On planet Mars==
2011 findings by the [[Opportunity (rover)|''Opportunity'']] rover on the planet [[Mars]] show a form of calcium sulfate in a vein on the surface. Images suggest the mineral is [[gypsum]].<ref>{{cite web|title=NASA Mars Opportunity rover finds mineral vein deposited by water|url=http://www.jpl.nasa.gov/news/news.php?release=2011-377&cid=release_2011-377&msource=11377&tr=y&auid=9976954|publisher=NASA Jet Propulsion Laboratory|access-date=April 23, 2013|date=December 7, 2011}}</ref>
 
==See also==