Skip to main content
Chemistry LibreTexts

Calcium Sulfate

Calcium sulfate, CaSO4, is a common laboratory and industrial chemical and an often used material in the building trade. It occurs naturally in various forms, which differ in their crystal water content: gypsum (CaSO4·2H2O), the hemihydrate (CaSO4·0.5H2O) also known as plaster of Paris, and the anhydrite. Despite its name the anhydrite is not always entirely devoid of water, the water content ranges from 0.0 to 0.05 mol-percent.

The main sources of calcium sulfate are naturally occurring minerals (gypsum and anhydrite). World production of natural gypsum is about 100 million tones per annum. Besides the natural sources, calcium sulfate is also produced as a by-product, mainly from the desulfurization of exhaust gases of fossil-fuel power stations.


Gypsum, CaSO4·2H2O, is thermodynamically stable in aqueous solutions below 42°C, while anhydrite, CaSO4, is stable above 42°. Thus gypsum crystallizes in aqueous solutions at low temperatures, while anhydrite crystallizes at higher temperatures. The hemihydrate is meta-stable.

Alkali and alkaline earth elements form double and triple salts with calcium sulfate, e.g. CaSO4K2SO4H2O, or 2CaSO4MgSO4K2SO42H2O

Dehydration of Gypsum

When heating gypsum to between 80 and 180°C it loses increasing amounts of water, forming first the hemihydrate and later the anhydrite:

CaSO4·2H2O + heat CaSO4·½H2O + 1½H2O (steam)
CaSO4·½H2O + heat CaSO4 + ½H2O (steam)

Depending on the humidity of the atmosphere during calcination, the structure of the resulting hemihydrate may be either coarse-crystalline (forming plaster gypsum under wet conditions) or fine-crystalline (stucco gypsum under dry conditions). Above 180 °C the anhydrite forms (first the γ-anhydrite, and at temperatures up to 800 °C the β-anhydrite). At temperatures between 800 and 1000 °C calcium sulfate partially decomposes into calcium oxide (CaSO4 CaO + SO3).

When mixed with water at ambient temperatures, calcined gypsum quickly reverts to the preferred dihydrate form, developing an interwoven network of gypsum crystals. This re-hydration reaction is exothermic and is responsible for the ease with which gypsum can be cast into various shapes.