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Definition of GypsumGypsum ( CaSO4·2H2O) is a natural monoclinic minera, Its main chemical component is calcium sulfate hydrate, which is widely distributed in the salt lake sediments formed by evaporation and widely used as industrial materials and building materials.
History of GypsumThe English word for plaster is 'Gypsum', and German is 'Gyps'. It all comes from the Greek γύψος (gypsos), and then the Latin word is 'gypsus'. At that time, it didn't mean gypsumin the modern sense, but meant something like moonstone.
Gypsum was used as a building material in the Neolithic Age and was used for interior decoration in Anatolia (now in Turkey) in BC. Evidence of the use of plaster was later found in Sumir and Babylon sites, such as Jericho in BC (now in Israel) and Uluk in BC (now in Iraq). The Pyramid of Khufu and the Sphinx, built in BC, used gypsum mortar as a cementitious material to bond and masonry stones.
Properties of GypsumGypsum is a very common soft sulfate mineral, which can be easily identified by its hardness, cleavage and solubility in water:
PropertiesValuePropertiesValueNameGypsumMelting''FormulaCaSO4·2H2OSolubilitysoluble in waterMolecular172CleavagePerfectColourWhite, colorless, or yellow-redHardness2 mohsLustreVitreous, Silky, PearlyTenacityFlexibleTransparencyTransparent, Translucent, OpaqueDensity2.31'2.33 g/cm3StreakWhiteCrystal StatePlate, fibrous, bulk or fine grainedCrystalMonoclinicApplicationArchitectural, MedicalClassification of Gypsum
Gypsum usually refers to two kinds of minerals: raw gypsum and anhydrite.
Raw Gypsum is calcium sulfate dihydrate ((Ca (SO4) 2H2O), also known as gypsum dihydrate, gypsum or gypsum, composition CaO (32.6%), SO3 (46.5%), H2O+ (20.9%), monoclinic system, crystal is plate-like, usually dense block or fiber, white or gray, red, brown, vitreous or silky luster, Mohs hardness is 2, density 2.3g/cm3.
Anhydrite is anhydrous calcium sulfate (Ca (SO4)), theoretical component CaO (41.2%), SSO3 (58.8%), orthorhombic system, crystal is plate, usually dense block or granular, white, grayish white, vitreous luster, Morse hardness is 3 ' 3.5, density 2.8~3.0g/cm3.
Raw gypsum and anhydrite are often produced together, and anhydrite can be formed by calcining gypsum at 400 ' 500 °C.
How is Gypsum Formed
Gypsum is a widely distributed mineral, which is mainly formed by sedimentation and weathering, and a few are found in hydrothermal sulphide deposits. Gypsum usually can be fond in the form of crystals or deposits beds.
Gypsum formed in sea basins and lake basins is formed by evaporation of brine or hydration of anhydrite; symbiosis with anhydrite, gypsum, etc. It is layered or lenticular in the interlayer of limestone, red shale, marl and sandy clay. The gypsum in the oxidation zone of sulphide deposits is mainly caused by sulfides.
If you are looking for more details, kindly visit Gypsum powder processing.
Distribution of Gypsum
The world's largest producer of gypsum is the United States. In the United States, gypsum deposits are distributed in 22 states with a total of 69 mines, with the largest producing area in Fort Dodge, Iowa, followed by Canada. France takes the lead in European gypsum production, followed by Germany, the United Kingdom and Spain.
Use of Gypsum
Gypsum is a widely used industrial material and building material. Gypsum (CaSO4 ·2H2O) can be calcined and grinded to obtain β-type hemihydrate gypsum (2CaSO4 ·H2O), that is, building gypsum, also known as cooked gypsum or plaster. The model gypsum can be obtained when the calcination temperature is 190 °C, and its fineness and whiteness are higher than that of building gypsum. If raw gypsum is calcined at 400 °C or above 800 °C, floor gypsum can be obtained, its setting and hardening are slow, but the strength, wear resistance and water resistance of hardened gypsum are better than that of ordinary building gypsum.
In addition, gypsum can also be used in the manufacture of cement, sulfuric acid, soil improvers, food coagulants, pesticide diluents as well as medical and cosmetology.
How is Gypsum Processed
The raw material of gypsum powder is natural gypsum ore, and the production process of gypsum powder is mainly divided into 5 stages: crushing, screening, grinding, calcination, storage and transportation.
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gypsum being a hazaardous mineral
No RER. Gypsum is a non-hazardous mineral.
Pure gypsum is a white rock but sometimes impurities colour it grey,
brown or pink. Its scientific name is calcium sulphate dihydrate and
its chemical formula is CaSO42H2O. This means that, for every
molecule of gypsum, there are two molecules of water.
If a piece of gypsum is ground to powder and heated, it will lose
about three quarters of its water. If this powder is then mixed with
water, the paste or slurry will set rock hard. The
chemically-combined water, previously removed, has re-combined and
the material has reverted to the original composition of the rock.
The powder is called hemi-hydrate gypsum plaster (Plaster of Paris).
Gypsum plaster has been used in buildings for literally thousands of
years.
Gypsum is found in every continent of the world.
From 1st April the guidance on landfill changed. Visible gypsum
waste can no longer be disposed to general landfill, but must go to
a separate cell for non-hazardous high-sulphate material. This is
because gypsum mixed with waste organic material can give off
hydrogen sulphide gas (bad eggs smell).
Bottom line Ms RER - Gypsum is a non-hazardous mineral.
Please check your info.!
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