·Measurements have been made of the rate of dehydration of desulphurized gypsum with particle diameters in the range of 35 67 μm in a fluidized bed reactor Experiments were carried out at bed temperatures of 100 to 170°C The fluidizing gases were air with water vapour pressures of between atm and atm and carbon dioxide The results show
·Gypsum calcium sulfate dihydrate CaSO 4 ·2H 2 O is the most aqueous phase in the system CaSO 4 H 2 O and besides anhydrite II the stable phase under ambient atmospheric conditions With increasing temperature gypsum starts to dehydrate and form calcium sulfates with lower H 2 O content The dehydration process proceeds stepwise and
·Calcium sulphate dihydrate CaSO4·2H2O or gypsum is used widely as building material because of its excellent fire resistance aesthetics and low price Hemihydrate occurs in two formations of α and β type Among them β hemihydrate is mainly used to produce gypsum plasterboard since the hydration product of the α hemihydrate is too brittle to be used
·Gypsum board dehydration Gypsum board dehydration takes place at the temperature range between ∼80 °C and 250 °C depending on the heating rate and the composition of the gypsum board [1] [10] [16] [17] During this process the chemically bound water dissociates from the crystal mesh and together with the free moisture content evaporates
·In this work we have reinvestigated the thermal degradation kinetics of synthetic gypsum CaSO4·2H2O using a novel approach based on peak deconvolution followed by the application of Model Free isoconversional method Gypsum was prepared using wet chemical route and characterized by conventional X ray diffraction in situ high temperature X
·As one of the extensively used inorganic cementitious material hemihydrate gypsum HH CaSO 4 · 2 O has two forms namely β HH and α HH β phase is a dehydration product of calcium sulfate dihydrate DH CaSO 4 ·2H 2 O in dry air at 105 180 °C and has a longer history of application whilst α HH can be produced by wet calcination
·DOI /0040 6031 95 02819 6 Corpus ID 98276387; The thermal dehydration of natural gypsum and pure calcium sulphate dihydrate gypsum article{HudsonLamb1996TheTD title={The thermal dehydration of natural gypsum and pure calcium sulphate dihydrate gypsum } author={D L Hudson Lamb and Christien A Strydom
·temperature dehydrated gypsum rock was treated with different hydration time and the gypsum rock samples in three states were subjected to ultrasonic test density test and uniaxial compression test The results show that the main components of natural gypsum minerals were gypsum dihydrate 71% dolomite 27% and potassium chloride 2% The
·The process of rehydration of calcium sulphate hemihydrate CaSO4 to the crystallization of gypsum which is chemically known as calcium sulphate dihydrate CaSO4 2H2O is based on the
Gypsum precipitates from aqueous solution under ambient conditions where it is the thermodynamically stable phase of calcium sulfate at temperatures below 40 60°C 1 2 11 12 Anhydrite becomes
Gypsum calcium sulfate dihydrate is one of the most used inorganic binding materials in the world During calcination calcium sulfate subhydrates are formed and for technical reasons are mixed with water to form dihydrate again Therefore the dehydration process of gypsum and the rehydration of hemihydrate were investigated
·Dihydrate gypsum is the dominant phase composition in PG it is a stable phase at room temperature but can be converted into α hemihydrate gypsum PG was subjected to calcination at relatively low temperatures and the effect of calcination temperature and time on dehydration behaviour of PG are shown in Fig 4 The crystal water content
Abstract Gypsum calcium sulfate dihydrate is one of the most used inorganic binding materials in the world During calcination calcium sulfate subhydrates are formed and for technical reasons
·The remediation of groundwater containing arsenic is a problem that has been addressed using adsorption processes with granulated materials in columns but the remediation itself could be improved
Keywords Gypsum Hemihydrate Soluble anhydrite Dehydration In situ high temperature synchrotron X ray diffraction INTRODUCTION Calcium sulfate dihydrate gypsum CaSO 4·2H 2O is the most common sulfate mineral Therefore considerable attention has been paid to the dehydration of gypsum Numerous studies on the mechanisms and products of
THE differential thermograms of calcium sulphate dihydrates gypsums show two relatively large endothermic effects in close sequence below 250° C There is general agreement1 2 that these two effects represent the two step decomposition of the dihydrate to hemihydrate and to soluble anhydrite A third small endothermic effect which is always associated with the second
·This β anhydrite is considered to be insoluble; meaning it cannot be converted back to dihydrate [3 7] At temperatures greater than 190 °C the formation of soluble anhydrite occurs followed by an insoluble anhydrite at higher temperature The dehydration mechanism of gypsum yields a mixture of hemihydrate and anhydrite [3 7] In
·In this work dehydration of CaSO 4 ·2H 2 O and CaSO 4 · 2 O in stagnant air was studied by thermo Raman spectroscopy from 25 to 300°C The composition could be identified directly from the Raman spectra by comparing with the known Raman spectra of CaSO 4 ·2H 2 O CaSO 4 · 2 O and CaSO Raman spectra indicated that dehydration
·gypsum contain both physically and chemically bound water Calcined gypsum hemihydrate CaSO4 · ½ H2O can be produced by various technologies Nowadays still relatively new but already very promising seems to be its production using the dehydration of waste flue gas desulfurization FGD gypsum dihydrate CaSO4 · 2H2O at the
·The dehydration behaviors of FGD gypsums from three power plants were investigated at N2 atmosphere autogenous and negligible partial pressure of water $$ P {{{text{H}} { 2} {text{O}}}} $$ in non isothermal and isothermal condition The dehydration of gypsum proceeded through one step CaSO4·2H2O → γ CaSO4 γ anhydrite or two
·In this work we have reinvestigated the thermal degradation kinetics of synthetic gypsum CaSO4·2H2O using a novel approach based on peak deconvolution followed by the application of Model Free isoconversional method Gypsum was prepared using wet chemical route and characterized by conventional X ray diffraction in situ high temperature X
·the dehydration of gypsum 𝛽 gypsum 3 hours at a temperature of 160 180 ° C 𝛼 gypsum 6 8 hours at a temperature of 124 ° C [ 4] Heating by m eans of microwave ultra high
·Certain concentration H can combine with the crystal water to form the H 3 O influencing the stability of the crystal water in dihydrate so that can be completely removed under lower this paper introduces a method wherein sulfuric acid is employed as a medium facilitating direct dry mixing and low calcination temperatures to produce anhydrite II
·The dehydration of gypsum to hemihydrate has been studied for decades because it is an important model reaction for understanding fluid triggered earthquakes and due to the global use of plaster