Gypsum

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Gypsum
Gypse Caresse.jpg
General
CategorySulfate minerals
Formula
(repeating unit)
CaSO4·2H2O
IMA symbolGp[1]
Strunz classification7.CD.40
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
H-M symbol: (2/m)
Space groupMonoclinic
Space group: I2/a
Unit cella = 5.679(5), b = 15.202(14)
c = 6.522(6) Å; β = 118.43°; Z = 4
Identification
ColorColorless (in transmitted light) to white; often tinged other hues due to impurities; may be yellow, tan, blue, pink, dark brown, reddish brown or gray
Crystal habitMassive, flat. Elongated and generally prismatic crystals
TwinningVery common on {110}
CleavagePerfect on {010}, distinct on {100}
FractureConchoidal on {100}, splintery parallel to [001]
TenacityFlexible, inelastic
Mohs scale hardness1.5–2 (defining mineral for 2)
LusterVitreous to silky, pearly, or waxy
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity2.31–2.33
Optical propertiesBiaxial (+)
Refractive indexnα = 1.519–1.521
nβ = 1.522–1.523
nγ = 1.529–1.530
Birefringenceδ = 0.010
PleochroismNone
2V angle58°
Fusibility5
SolubilityHot, dilute HCl
References[2][3][4]
Major varieties
Satin sparPearly, fibrous masses
SeleniteTransparent and bladed crystals
AlabasterFine-grained, slightly colored

Gypsum is a soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula CaSO4·2H2O.[4] It is widely mined and is used as a fertilizer and as the main constituent in many forms of plaster, blackboard or sidewalk chalk, and drywall. A massive fine-grained white or lightly tinted variety of gypsum, called alabaster, has been used for sculpture by many cultures including Ancient Egypt, Mesopotamia, Ancient Rome, the Byzantine Empire, and the Nottingham alabasters of Medieval England. Gypsum also crystallizes as translucent crystals of selenite. It forms as an evaporite mineral and as a hydration product of anhydrite.

The Mohs scale of mineral hardness defines gypsum as hardness value 2 based on scratch hardness comparison.

Etymology and history[edit]

The word gypsum is derived from the Greek word γύψος (gypsos), "plaster".[5] Because the quarries of the Montmartre district of Paris have long furnished burnt gypsum (calcined gypsum) used for various purposes, this dehydrated gypsum became known as plaster of Paris. Upon adding water, after a few dozen minutes, plaster of Paris becomes regular gypsum (dihydrate) again, causing the material to harden or "set" in ways that are useful for casting and construction.[6]

Gypsum was known in Old English as spærstān, "spear stone", referring to its crystalline projections. (Thus, the word spar in mineralogy is by way of comparison to gypsum, referring to any non-ore mineral or crystal that forms in spearlike projections). In the mid-18th century, the German clergyman and agriculturalist Johann Friderich Mayer investigated and publicized gypsum's use as a fertilizer.[7] Gypsum may act as a source of sulfur for plant growth, and in the early 19th century, it was regarded as an almost miraculous fertilizer. American farmers were so anxious to acquire it that a lively smuggling trade with Nova Scotia evolved, resulting in the so-called "Plaster War" of 1820.[8]

Physical properties[edit]

Gypsum crystals are soft enough to bend under pressure of the hand. Sample on display at Musée cantonal de géologie de Lausanne.

Gypsum is moderately water-soluble (~2.0–2.5 g/L at 25 °C)[9] and, in contrast to most other salts, it exhibits retrograde solubility, becoming less soluble at higher temperatures. When gypsum is heated in air it loses water and converts first to calcium sulfate hemihydrate, (bassanite, often simply called "plaster") and, if heated further, to anhydrous calcium sulfate (anhydrite). As with anhydrite, the solubility of gypsum in saline solutions and in brines is also strongly dependent on NaCl (common table salt) concentration.[9]

The structure of gypsum consists of layers of calcium (Ca2+) and sulfate (SO2−4) ions tightly bound together. These layers are bonded by sheets of anion water molecules via weaker hydrogen bonding, which gives the crystal perfect cleavage along the sheets (in the {010} plane).[4][10]

Crystal varieties[edit]

Gypsum occurs in nature as flattened and often twinned crystals, and transparent, cleavable masses called selenite. Selenite contains no significant selenium; rather, both substances were named for the ancient Greek word for the Moon.

Selenite may also occur in a silky, fibrous form, in which case it is commonly called "satin spar". Finally, it may also be granular or quite compact. In hand-sized samples, it can be anywhere from transparent to opaque. A very fine-grained white or lightly tinted variety of gypsum, called alabaster, is prized for ornamental work of various sorts. In arid areas, gypsum can occur in a flower-like form, typically opaque, with embedded sand grains called desert rose. It also forms some of the largest crystals found in nature, up to 12 m (39 ft) long, in the form of selenite.[11]

Occurrence[edit]

Gypsum is a common mineral, with thick and extensive evaporite beds in association with sedimentary rocks. Deposits are known to occur in strata from as far back as the Archaean eon.[12] Gypsum is deposited from lake and sea water, as well as in hot springs, from volcanic vapors, and sulfate solutions in veins. Hydrothermal anhydrite in veins is commonly hydrated to gypsum by groundwater in near-surface exposures. It is often associated with the minerals halite and sulfur. Gypsum is the most common sulfate mineral.[13] Pure gypsum is white, but other substances found as impurities may give a wide range of colors to local deposits.

Because gypsum dissolves over time in water, gypsum is rarely found in the form of sand. However, the unique conditions of the White Sands National Park in the US state of New Mexico have created a 710 km2 (270 sq mi) expanse of white gypsum sand, enough to supply the US construction industry with drywall for 1,000 years.[14] Commercial exploitation of the area, strongly opposed by area residents, was permanently prevented in 1933 when President Herbert Hoover declared the gypsum dunes a protected national monument.

Gypsum is also formed as a by-product of sulfide oxidation, amongst others by pyrite oxidation, when the sulfuric acid generated reacts with calcium carbonate. Its presence indicates oxidizing conditions. Under reducing conditions, the sulfates it contains can be reduced back to sulfide by sulfate-reducing bacteria. This can lead to accumulation of elemental sulfur in oil-bearing formations,[15] such as salt domes,[16] where it can be mined using the Frasch process[17] Electric power stations burning coal with flue gas desulfurization produce large quantities of gypsum as a byproduct from the scrubbers.

Orbital pictures from the Mars Reconnaissance Orbiter (MRO) have indicated the existence of gypsum dunes in the northern polar region of Mars,[18] which were later confirmed at ground level by the Mars Exploration Rover (MER) Opportunity.[19]

Mining[edit]

Estimated production of Gypsum in 2015
(thousand metric tons)[20]
Country Production Reserves
China 132,000
Iran 22,000 1,600
Thailand 12,500
United States 11,500 700,000
Turkey 10,000
Spain 6,400
Mexico 5,300
Japan 5,000
Russia 4,500
Italy 4,100
India 3,500 39,000
Australia 3,500
Oman 3,500
Brazil 3,300 290,000
France 3,300
Canada 2,700 450,000
Saudi Arabia 2,400
Algeria 2,200
Germany 1,800 450,000
Argentina 1,400
Pakistan 1,300
United Kingdom 1,200 55,000
Other countries 15,000
World total 258,000

Commercial quantities of gypsum are found in the cities of Araripina and Grajaú in Brazil; in Pakistan, Jamaica, Iran (world's second largest producer), Thailand, Spain (the main producer in Europe), Germany, Italy, England, Ireland, Canada[21] and the United States. Large open pit quarries are located in many places including Fort Dodge, Iowa, which sits on one of the largest deposits of gypsum in the world,[22] and Plaster City, California, United States, and East Kutai, Kalimantan, Indonesia. Several small mines also exist in places such as Kalannie in Western Australia, where gypsum is sold to private buyers for additions of calcium and sulfur as well as reduction of aluminum toxicities on soil for agricultural purposes.

Crystals of gypsum up to 11 m (36 ft) long have been found in the caves of the Naica Mine of Chihuahua, Mexico. The crystals thrived in the cave's extremely rare and stable natural environment. Temperatures stayed at 58 °C (136 °F), and the cave was filled with mineral-rich water that drove the crystals' growth. The largest of those crystals weighs 55 tonnes (61 short tons) and is around 500,000 years old.[23]

Synthesis[edit]

Synthetic gypsum is produced as a waste product or by-product in a range of industrial processes.

Desulfurization[edit]

Flue gas desulfurization gypsum (FGDG) is recovered at some coal-fired power plants. The main contaminants are Mg, K, Cl, F, B, Al, Fe, Si, and Se. They come both from the limestone used in desulfurization and from the coal burned. This product is pure enough to replace natural gypsum in a wide variety of fields including drywalls, water treatment, and cement set retarder. Improvements in flue gas desulfurization have greatly reduced the amount of toxic elements present.[24]

Desalination[edit]

Gypsum precipitates onto brackish water membranes, a phenomenon known as mineral salt scaling, such as during brackish water desalination of water with high concentrations of calcium and sulfate. Scaling decreases membrane life and productivity.[25] This is one of the main obstacles in brackish water membrane desalination processes, such as reverse osmosis or nanofiltration. Other forms of scaling, such as calcite scaling, depending on the water source, can also be important considerations in distillation, as well as in heat exchangers, where either the salt solubility or concentration can change rapidly.

A new study has suggested that the formation of gypsum starts as tiny crystals of a mineral called bassanite (CaSO4·0.5H2O).[26] This process occurs via a three-stage pathway:

  1. homogeneous nucleation of nanocrystalline bassanite;
  2. self-assembly of bassanite into aggregates, and
  3. transformation of bassanite into gypsum.

Refinery waste[edit]

The production of phosphate fertilizers requires breaking down calcium-containing phosphate rock with acid, producing calcium sulfate waste known as phosphogypsum (PG). This form of gypsum is contaminated by impurities found in the rock, namely fluoride, silica, radioactive elements such as radium, and heavy metal elements such as cadmium.[27] Similarly, production of titanium dioxide produces titanium gypsum (TG) due to neutralization of excess acid with lime. The product is contaminated with silica, fluorides, organic matters, and alkalis.[28]

Impurities in refinery gypsum waste have, in many cases, prevented them from being used as normal gypsum in fields such as construction. As a result, waste gypsum is stored in stacks indefinitely, with significant risk of leaching their contaminants into water and soil.[27] To reduce the accumulation and ultimately clear out these stacks, research is underway to find more applications for such waste products.[28]

Occupational safety[edit]

NFPA 704
fire diamond
Gypsum

People can be exposed to gypsum in the workplace by breathing it in, skin contact, and eye contact. Calcium sulfate per se is nontoxic and is even approved as a food additive,[30] but as powdered gypsum, it can irritate skin and mucous membranes.[31]

United States[edit]

The Occupational Safety and Health Administration (OSHA) has set the legal limit (permissible exposure limit) for gypsum exposure in the workplace as TWA 15 mg/m3 for total exposure and TWA 5 mg/m3 for respiratory exposure over an 8-hour workday. The National Institute for Occupational Safety and Health (NIOSH) has set a recommended exposure limit (REL) of TWA 10 mg/m3 for total exposure and TWA 5 mg/m3 for respiratory exposure over an 8-hour workday.[31]

Uses[edit]

Map of gypsum deposits in northern Ohio, black squares indicate the location of deposits, from "Geography of Ohio", 1923

Gypsum is used in a wide variety of applications:

Construction industry[edit]

  • Gypsum board[32] is primarily used as a finish for walls and ceilings, and is known in construction as plasterboard, "sheetrock", or drywall. Gypsum provides a degree of fire-resistance to these materials and glass fibers are added to their composition to accentuate this effect. Gypsum has little heat conductivity, giving its plaster some insulative properties.[33]
  • Gypsum blocks are used like concrete blocks in building construction.
  • Gypsum mortar is an ancient mortar used in building construction.
  • A component of Portland cement used to prevent flash setting (too rapid hardening) of concrete.

Agriculture[edit]

Modeling, sculpture and art[edit]

  • Plaster for casting moulds and modeling.
  • As alabaster, a material for sculpture, it was used especially in the ancient world before steel was developed, when its relative softness made it much easier to carve.[41] During the Middle Ages and Renaissance, it was preferred even to marble.[42]
  • In the medieval period, scribes and illuminators used it as an ingredient in gesso, which was applied to illuminated letters and gilded with gold in illuminated manuscripts.[43]

Food and drink[edit]

  • A tofu (soy bean curd) coagulant, making it ultimately a significant source of dietary calcium.[44]
  • Adding hardness to water used for brewing.[45]
  • Used in baking as a dough conditioner, reducing stickiness, and as a baked-goods source of dietary calcium.[46] The primary component of mineral yeast food.[47]
  • Used in mushroom cultivation to stop grains from clumping together.

Medicine and cosmetics[edit]

Other[edit]

  • An alternative to iron oxide in some thermite mixes.[50]
  • Tests have shown that gypsum can be used to remove pollutants such as lead[51] or arsenic[52][53] from contaminated waters.

Gallery[edit]

See also[edit]

References[edit]

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C., eds. (2003). "Gypsum" (PDF). Handbook of Mineralogy. Vol. V (Borates, Carbonates, Sulfates). Chantilly, VA, US: Mineralogical Society of America. ISBN 978-0962209703.
  3. ^ Gypsum. Mindat
  4. ^ a b c Klein, Cornelis; Hurlbut, Cornelius S., Jr. (1985), Manual of Mineralogy (20th ed.), John Wiley, pp. 352–353, ISBN 978-0-471-80580-9
  5. ^ "Compact Oxford English Dictionary: gypsum". Archived from the original on 19 July 2012.
  6. ^ Szostakowski, B.; Smitham, P.; Khan, W.S. (17 April 2017). "Plaster of Paris–Short History of Casting and Injured Limb Immobilzation". The Open Orthopaedics Journal. 11: 291–296. doi:10.2174/1874325001711010291. ISSN 1874-3250. PMC 5420179. PMID 28567158.
  7. ^ See:
    • Thaer, Albrecht Daniel; Shaw, William, trans.; Johnson, Cuthbert W., trans. (1844). The Principles of Agriculture. Vol. 1. London, England: Ridgway. pp. 519–520.
    • Klaus Herrmann (1990), "Mayer, Johann Friedrich", Neue Deutsche Biographie (in German), vol. 16, Berlin: Duncker & Humblot, pp. 544–545; (full text online) From p. 544: " … er bewirtschaftete nebenbei ein Pfarrgüttchen, … für die Düngung der Felder mit dem in den nahen Waldenburger Bergen gefundenen Gips einsetzte." ( … he also managed a small parson's estate, on which he repeatedly conducted agricultural experiments. In 1768, he first published the fruits of his experiences during this time as "Instruction about Gypsum", in which he espoused the fertilizing of fields with the gypsum that was found in the nearby Waldenburg mountains.)
    • Beckmann, Johann (1775). Grundsätze der deutschen Landwirthschaft [Fundamentals of German Agriculture] (in German) (2nd ed.). Göttingen, (Germany): Johann Christian Dieterich. p. 60. From p. 60: "Schon seit undenklichen Zeiten … ein Gewinn zu erhalten seyn wird." (Since times immemorial, in our vicinity, in the ministry of Niedeck [a village southeast of Göttingen], one has already made this use of gypsum; but Mr. Mayer has the merit to have made it generally known. In the History of Farming in Kupferzell, he had depicted a crushing mill (p. 74), in order to pulverize gypsum, from which a profit has been obtained, albeit with difficulty.)
    • Mayer, Johann Friderich (1768). Lehre vom Gyps als vorzueglich guten Dung zu allen Erd-Gewaechsen auf Aeckern und Wiesen, Hopfen- und Weinbergen [Instruction in gypsum as an ideal good manure for all things grown in soil on fields and pastures, hops yards and vineyards] (in German). Anspach, (Germany): Jacob Christoph Posch.
  8. ^ Smith, Joshua (2007). Borderland smuggling: Patriots, loyalists, and illicit trade in the Northeast, 1780–1820. Gainesville, FL: UPF. pp. passim. ISBN 978-0-8130-2986-3.
  9. ^ a b Bock, E. (1961). "On the solubility of anhydrous calcium sulphate and of gypsum in concentrated solutions of sodium chloride at 25 °C, 30 °C, 40 °C, and 50 °C". Canadian Journal of Chemistry. 39 (9): 1746–1751. doi:10.1139/v61-228.
  10. ^ Mandal, Pradip K; Mandal, Tanuj K (2002). "Anion water in gypsum (CaSO4·2H2O) and hemihydrate (CaSO4·1/2H2O)". Cement and Concrete Research. 32 (2): 313. doi:10.1016/S0008-8846(01)00675-5.
  11. ^ García-Ruiz, Juan Manuel; Villasuso, Roberto; Ayora, Carlos; Canals, Angels; Otálora, Fermín (2007). "Formation of natural gypsum megacrystals in Naica, Mexico" (PDF). Geology. 35 (4): 327–330. Bibcode:2007Geo....35..327G. doi:10.1130/G23393A.1. hdl:10261/3439.
  12. ^ Cockell, C. S.; Raven, J. A. (2007). "Ozone and life on the Archaean Earth". Philosophical Transactions of the Royal Society A. 365 (1856): 1889–1901. Bibcode:2007RSPTA.365.1889C. doi:10.1098/rsta.2007.2049. PMID 17513273. S2CID 4716.
  13. ^ Deer, W.A.; Howie, R.A.; Zussman, J. (1966). An Introduction to the Rock Forming Minerals. London: Longman. p. 469. ISBN 978-0-582-44210-8.
  14. ^ Abarr, James (7 February 1999). "Sea of sand". The Albuquerque Journal. Archived from the original on 30 June 2006. Retrieved 27 January 2007.
  15. ^ Machel, H.G (April 2001). "Bacterial and thermochemical sulfate reduction in diagenetic settings — old and new insights". Sedimentary Geology. 140 (1–2): 143–175. Bibcode:2001SedG..140..143M. doi:10.1016/S0037-0738(00)00176-7.
  16. ^ Sassen, Roger; Chinn, E.W.; McCabe, C. (December 1988). "Recent hydrocarbon alteration, sulfate reduction and formation of elemental sulfur and metal sulfides in salt dome cap rock". Chemical Geology. 74 (1–2): 57–66. Bibcode:1988ChGeo..74...57S. doi:10.1016/0009-2541(88)90146-5.
  17. ^ Wolfgang Nehb, Karel Vydra. "Sulfur". Ullmann's Encyclopedia of Industrial Chemistry. Weinheim: Wiley-VCH. doi:10.1002/14356007.a25_507.pub2.
  18. ^ High-resolution Mars image gallery. University of Arizona
  19. ^ NASA Mars Rover Finds Mineral Vein Deposited by Water, NASA, 7 December 2011.
  20. ^ "GYPSUM" (PDF). U.S. Geological Survey.
  21. ^ "Mines, mills and concentrators in Canada". Natural Resources Canada. 24 October 2005. Archived from the original on 13 March 2005. Retrieved 27 January 2007.
  22. ^ The Hutchinson Unabridged Encyclopedia with Atlas and Weather Guide. Helion. 2018 – via Credo Reference.
  23. ^ Alleyne, Richard (27 October 2008). "World's largest crystal discovered in Mexican cave". The Telegraph. London. Retrieved 6 June 2009.
  24. ^ Koralegedara, NH; Pinto, PX; Dionysiou, DD; Al-Abed, SR (1 December 2019). "Recent advances in flue gas desulfurization gypsum processes and applications - A review". Journal of Environmental Management. 251: 109572. doi:10.1016/j.jenvman.2019.109572. PMC 7396127. PMID 31561139.
  25. ^ Uchymiak, Michal; Lyster, Eric; Glater, Julius; Cohen, Yoram (April 2008). "Kinetics of gypsum crystal growth on a reverse osmosis membrane". Journal of Membrane Science. 314 (1–2): 163–172. doi:10.1016/j.memsci.2008.01.041.
  26. ^ Van Driessche, A.E.S.; Benning, L. G.; Rodriguez-Blanco, J. D.; Ossorio, M.; Bots, P.; García-Ruiz, J. M. (2012). "The role and implications of bassanite as a stable precursor phase to gypsum precipitation". Science. 336 (6077): 69–72. Bibcode:2012Sci...336...69V. doi:10.1126/science.1215648. PMID 22491851. S2CID 9355745.
  27. ^ a b Tayibi, Hanan; Choura, Mohamed; López, Félix A.; Alguacil, Francisco J.; López-Delgado, Aurora (2009). "Environmental Impact and Management of Phosphogypsum". Journal of Environmental Management. 90 (8): 2377–2386. doi:10.1016/j.jenvman.2009.03.007. hdl:10261/45241. PMID 19406560.
  28. ^ a b Zhang, Y; Wang, F; Huang, H; Guo, Y; Li, B; Liu, Y; Chu, PK (2016). "Gypsum blocks produced from TiO2 production by-products" (PDF). Environmental Technology. 37 (9): 1094–100. doi:10.1080/09593330.2015.1102329. PMID 26495867. S2CID 28458281.
  29. ^ Michigan Gypsum. "MATERIAL SAFETY DATA SHEET Gypsum (Calcium Sulfate Dihydrate)" (PDF). Consumer Information. NorthCentral Missouri College. Retrieved 21 November 2021.
  30. ^ "Compound Summary for CID 24497 - Calcium Sulfate". PubChem.
  31. ^ a b "CDC – NIOSH Pocket Guide to Chemical Hazards – Gypsum". www.cdc.gov. Retrieved 3 November 2015.
  32. ^ *Complimentary list of MasterFormat 2004 Edition numbers and titles (large PDF document)
  33. ^ Bonewitz, Ronald (2008). Rock and Gem: The Definitive Guide to Rocks, Minerals, Gems, and Fossils. United States: DK. p. 47.
  34. ^ Graham, Gerald S. (1938). "The Gypsum Trade of the Maritime Provinces: Its Relation to American Diplomacy and Agriculture in the Early Nineteenth Century". Agricultural History. 12 (3): 209–223. JSTOR 3739630.
  35. ^ a b "Gypsum as an agricultural product | Soil Science Society of America". www.soils.org.
  36. ^ Genesis and Management of Sodic (Alkali) Soils. (2017). (n.p.): Scientific Publishers.
  37. ^ Oster, J. D.; Frenkel, H. (1980). "The chemistry of the reclamation of sodic soils with gypsum and lime". Soil Science Society of America Journal. 44 (1): 41–45. Bibcode:1980SSASJ..44...41O. doi:10.2136/sssaj1980.03615995004400010010x.
  38. ^ Ley, Willy (October 1961). "The Home-Made Land". For Your Information. Galaxy Science Fiction. pp. 92–106.
  39. ^ Hogan, C. Michael (2007). "Knossos fieldnotes". Modern Antiquarian.
  40. ^ Durner, W.; Or, D. (2006). "Soil water potential measurement" (PDF). In Anderson, M.G. (ed.). Encyclopedia of hydrological sciences. John Wiley & Sons Ltd. ISBN 978-0471491033. Retrieved 23 May 2022.
  41. ^ Rapp, George (2009). "Soft Stones and Other Carvable Materials". Archaeomineralogy. Natural Science in Archaeology: 121–142. doi:10.1007/978-3-540-78594-1_6. ISBN 978-3-540-78593-4.
  42. ^ Kloppmann, W.; Leroux, L.; Bromblet, P.; Le Pogam, P.-Y.; Cooper, A. H.; Worley, N.; Guerrot, C.; Montech, A. T.; Gallas, A. M.; Aillaud, R. (7 November 2017). "Competing English, Spanish, and French alabaster trade in Europe over five centuries as evidenced by isotope fingerprinting". Proceedings of the National Academy of Sciences. 114 (45): 11856–11860. Bibcode:2017PNAS..11411856K. doi:10.1073/pnas.1707450114. PMC 5692548. PMID 29078309.
  43. ^ Brown, Michelle (1995). Understanding illuminated manuscripts : a guide to technical terms. Los Angeles, California. p. 58. ISBN 9780892362172.
  44. ^ Shurtleff, William (2000). Tofu & soymilk production : a craft and technical manual. Lafayette, CA: Soyfoods Center. ISBN 9781928914044.
  45. ^ Palmer, John. "Water Chemistry Adjustment for Extract Brewing". HowToBrew.com. Retrieved 15 December 2008.
  46. ^ "Calcium sulphate for the baking industry" (PDF). United States Gypsum Company. Archived from the original (PDF) on 4 July 2013. Retrieved 1 March 2013.
  47. ^ "Tech sheet for yeast food" (PDF). Lesaffre Yeast Corporation. Archived from the original (PDF) on November 2014. Retrieved 1 March 2013.
  48. ^ Austin, R.T. (March 1983). "Treatment of broken legs before and after the introduction of gypsum". Injury. 14 (5): 389–394. doi:10.1016/0020-1383(83)90089-X. PMID 6347885.
  49. ^ Drennon, David G.; Johnson, Glen H. (February 1990). "The effect of immersion disinfection of elastomeric impressions on the surface detail reproduction of improved gypsum casts". The Journal of Prosthetic Dentistry. 63 (2): 233–241. doi:10.1016/0022-3913(90)90111-O. PMID 2106026.
  50. ^ Govender, Desania R.; Focke, Walter W.; Tichapondwa, Shepherd M.; Cloete, William E. (20 June 2018). "Burn Rate of Calcium Sulfate Dihydrate–Aluminum Thermites". ACS Applied Materials & Interfaces. 10 (24): 20679–20687. doi:10.1021/acsami.8b04205. hdl:2263/66006. PMID 29842778. S2CID 206483977.
  51. ^ Astilleros, J.M.; Godelitsas, A.; Rodríguez-Blanco, J.D.; Fernández-Díaz, L.; Prieto, M.; Lagoyannis, A.; Harissopulos, S. (2010). "Interaction of gypsum with lead in aqueous solutions" (PDF). Applied Geochemistry. 25 (7): 1008. Bibcode:2010ApGC...25.1008A. doi:10.1016/j.apgeochem.2010.04.007.
  52. ^ Rodriguez, J. D.; Jimenez, A.; Prieto, M.; Torre, L.; Garcia-Granda, S. (2008). "Interaction of gypsum with As(V)-bearing aqueous solutions: Surface precipitation of guerinite, sainfeldite, and Ca2NaH(AsO4)2⋅6H2O, a synthetic arsenate". American Mineralogist. 93 (5–6): 928. Bibcode:2008AmMin..93..928R. doi:10.2138/am.2008.2750. S2CID 98249784.
  53. ^ Rodríguez-Blanco, Juan Diego; Jiménez, Amalia; Prieto, Manuel (2007). "Oriented Overgrowth of Pharmacolite (CaHAsO4⋅2H2O) on Gypsum (CaSO4⋅2H2O)". Cryst. Growth Des. 7 (12): 2756–2763. doi:10.1021/cg070222+.

External links[edit]