The mineral Gypsum precipitated some 100 to 200 million years ago when sea water evaporated. From a chemical point of view it is Calcium Sulphate Dihydrate (CaSO4,2H2O) deposited in sedimentary layers on the sea bed. Under high pressure and temperature Gypsum turns into Anhydrite (CaSO4).
Calcium Sulphate and its Release into Soil and Groundwater
Gypsum is a rock like mineral commonly found in the earth’s crust, extracted, processed and used by Man in construction or decoration in the form of plaster and alabaster since 9000 B.C. The facts show that calcium sulphate is a substance with no adverse health and environmental effects.
FGD Gypsum quality criteria parameters are determined in accordance with VGB Instruction Sheet "Analysis of FGDP Gypsum".
FGD Gypsum quality shall be such that it can be used for for the production of gypsum-based products which are equivalent to those made from natural gypsum.
Even though moulds are a fact of the day-to-day life, mould growth can be
eliminated by preventing the conditions which allows the spores (seeds) to
develop into moulds and by taking sensible prevention measures detailed in this
document. Basically, the key to mould is to control moisture impeding the
mould’s spores to come inside the building.
Gypsum plasters and plasterboards provide good fire protection in buildings due to the
unique behaviour of gypsum when exposed to fire. Pure gypsum (CaSO4.2H2O) contains
nearly 21% chemically combined water of crystallisation, and about 79% calcium sulphate, which is inert below a temperature of 1200°C.