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1.
Beta C2 S was hydrated at room temperature with and without added CaCl2 or C2 H5 OH by methods previously studied for the hydration of C3 S, i.e. paste, bottle, and ball-mill hydration. The amount of reacted β-C2 S, the Ca(OH)2 concentration in the liquid phase, the CaO/SiO2 molar ratio, and the specific surface area of the hydrate were investigated. A topochemical reaction occurs between water and β-C2 S, resulting in the appearance of solid Ca(OH)2 and a hydrated silicate with a CaO/SiO2 molar ratio of ≃1. As the liquid phase becomes richer in Ca(OH)2 , the first hydrate transforms to one with a higher CaO/SiO2 ratio. Addition of CaCl2 increases the reaction rate and the surface area of the hydrate but to a much lesser extent than in the hydration of C3 S, whereas C2 H6 OH strongly depresses the hydration rate of β-C2 S, as observed for C3 S hydration. 相似文献
2.
Hideki Ishida Kaori Sasaki Yoshihiko Okada Takeshi Mitsuda 《Journal of the American Ceramic Society》1992,75(9):2541-2546
The effect of curing temperature (40°, 60°, 80°C) on the hydration behavior of β-dicalcium silicate (β-C2 S) was investigated. The β-C2 S was obtained by decomposition of hillebrandite, Ca2 (SiO3 )(OH)2 , at 600°C, has a specific surface area of about 7 m2 /g, and is in the form of fibrous crystals. The dependence of the hydration reaction on temperature continues until the reaction is completed. The hydration is completed in 1 day at 80°C and in 14 days at 14°C. The hydration mechanism is different above and below 60°C, but at a given temperature, the reaction mechanism and the silicate anion structures of C-S-H do not change significantly from the initial to the late stages of the reaction. High curing temperature and long curing times after completion of reaction promote silicate polymerization. The Ca/Si ratio of C-S-H shows high values, being almost 2.0 above 60°C and 1.95 below 40°C. 相似文献
3.
Kaori Sasaki Hideki Ishida Yoshihiko Okada Takeshi Mitsuda 《Journal of the American Ceramic Society》1993,76(4):870-874
The hydration of β-C2 S prepared from hillebrandite [Ca2 (SiO3 )(OH)2 ] and having specific surface areas of 6.8, 5.5, and 3.1 m2 /g was investigated. Different specific areas were obtained by varying the dissociation temperature of hillebrandite. In addition, the hydration of β-C2 S synthesized from high-temperature solid-state reaction was also studied as a comparison. The specific surface area exerts a strong influence on the hydration rate, which increases as the surface area increases. The degree of influence changes with the reaction, becoming greater as hydration progresses. There is initially a linear relationship between specific area and the time required to complete a specific reaction. The specific surface area also affects the reaction mechanism. In the case of specific areas of 5.5 m2 /g or less, the reaction changes from a chemical reaction to a diffusion-controlled one, and the degree of reaction comes almost to a halt at 80% to 85%. The Ca/Si ratios of hydrate and the silicate anion structures were also investigated in this study. 相似文献
4.
Characterization of C-S-H from Highly Reactive β-Dicalcium Silicate Prepared from Hillebrandite 总被引:1,自引:1,他引:0
Yoshihiko Okada Hideki Ishida Kaori Sasaki J. Francis Young Takeshi Mitsuda 《Journal of the American Ceramic Society》1994,77(5):1313-1318
β-dicalcium silicate synthesized by thermal dissociation of hydrothermally prepared hillebrandite (Ca2 (SiO3 )(OH)2 ) exhibits extremely high hydration activity. Characterization of the hydrates obtained and investigation of the hydration mechanism was carried out with the aid of trimethylsilylation analysis, 29 Si magic angle spinning nuclear magnetic resonance, transmission electron microscopy selected area electron diffraction, and XRD. The silicate anion structure of C-S-H consisted mainly of a dimer and a single-chain polymer. Polymerization advances with increasing curing temperature and curing time. The C-S-H has an oriented fibrous structure and exhibits a 0.73-nm dreierketten in the longitudinal direction. On heating, the C-S-H dissociates to form β-C2 S. The temperature at which βC2 S begins to form decreases with increasing chain length of the C-S-H or as the Ca/Si ratio becomes higher. The high activity of β-C2 S is due to its large specific surface area and the fact that the hydration is chemical-reaction-rate-controlled until its completion. As a result, the hydration progresses in situ and C-S-H with a high Ca/Si ratio is formed. 相似文献
5.
Hideki Ishida Yoshihiko Okada Takeshi Mitsuda 《Journal of the American Ceramic Society》1992,75(2):359-363
The hydration behavior at 25°C of highly reactive β-dicalcium silicate synthesized from hillebrandite (Ca2 (SiO3 )(OH)2 ) was studied over a period of 7 to 224 d using 29 Si magic-angle spinning nuclear magnetic resonance (MAS NMR). The hydration product, C-S-H, contains Q2 and Q1 silicate tetrahedra, the chemical shifts of which are independent of the water/solid (w/s) ratio and curing time. Until the reaction is completed, the amounts of Q1 and Q2 formed are independent of the w/s ratio, being determined only by the degree of reaction. The ratio Q2 /Q1 increases as the reaction progresses and as the curing time becomes longer. From the values of Q2 /Q1 , it appears that the hydrate is a mixture of dimers and short single-chain polymers. The Ca/Si ratio of the hydrate is high, taking values close to 2.0, but the Ca/Si ratio does not influence the Q2 /Q1 ratio. It was also found that the NMR peak intensities allow quantitative assessment similar to XRD. 相似文献
6.
Reaction of Beta-Dicalcium Silicate and Tricalcium Silicate with Carbon Dioxide and Water Vapor 总被引:2,自引:0,他引:2
C. J. GOODBRAKE J. F. YOUNG R. L. BERGER 《Journal of the American Ceramic Society》1979,62(3-4):168-171
The carbonation-reaction kinetics of beta-dicalcium silicate (2CaO·SiO2 or β-C2 S) and tricalcium silicate (3CaO. SiO2 or C3 S) powders were determined as a function of material parameters and reaction conditions and an equation was developed which predicted the degree of reaction. The effect of relative humidity, partial pressure of CO2 , surface area, reaction temperature, and reaction time on the degree of reaction was determined. Carbonation followed a decreasing-volume, diffusion-controlled kinetic model. The activation energies for carbonation of β-C2 S and C3 S were 16.9 and 9.8 kcal/mol, respectively. Aragonite was the principal carbonate formed during the reaction and the rate of carbonate formation was coincident with depletion of the calcium silicates; C-S-H gel formation was minimal. 相似文献
7.
C. J. GOODBRAKE J. F. YOUNG R. L. BERGER 《Journal of the American Ceramic Society》1979,62(9-10):488-491
The carbonation of wetted powders of beta-dicalcium silicate (β·2CaO·SiO2 =β-C2 S) and tricalcium silicate (3CaO·SiO2 = C3 S) was studied as a function of reaction conditions. The water/solids ratio is an important parameter and there is an optimum value for each silicate. Relative humidity and the partial pressure of CO2 also strongly affect the reaction. The rate of carbonation can be conveniently represented by plotting the degree of carbonation against the logarithm of time. C-S-H and calcite are the initial reaction products. Subsequently, carbonation of the C-S-H produces silica gel, whereas aragonite may form if the system is allowed to dry out. 相似文献
8.
Sabine Thomas Karin Meise-Gresch Werner Müller-Warmuth Ivan Odler 《Journal of the American Ceramic Society》1993,76(8):1998-2004
9.
The effects of Al3+ , B3+ , P5+ , Fe3+ , S6+ , and K+ ions on the stability of the β-phase and its hydration rate were studied in reactive dicalcium silicate (C2 S, Ca2 SiO4 ) synthesized using the Pechini process. In particular, the dependences of the phase stability and degree of hydration on the calcination temperature (i.e., particle size) and the concentration of the stabilizing ions were investigated. The phase evolution in doped C2 S was determined using XRD, and the degree of hydration was estimated by the peak intensity ratio of the hydrates to the nonhydrates in 29 Si MAS NMR spectra. The stabilizing ability of the ions varied significantly, and the B3+ ions were quite effective in stabilizing the β-phase over a wide range of doping concentrations. The hydration results indicated that differently stabilized β-C2 S hydrated at different rates, and Al3+ - and B3+ -doped C2 S exhibited increased degree of hydration for all doping concentration ranges investigated. The effect of the doping concentration on degree of hydration was strongly dependent on the stabilizing ions. 相似文献
10.
Adrian R. Brough Christopher M. Dobson Ian G. Richardson Geoffrey W. Groves 《Journal of the American Ceramic Society》1994,77(2):593-596
Selective isotopic enrichment of SiO2 with 29 Si in a mixture with tricalcium silicate (C3 S) has allowed the Si from this phase to be effectively labeled during the course of the hydration reaction, thus isolating its contribution to the reaction. A double Q2 signal has been observed in 29 SI solid-state MAS NMR spectroscopy of C-S-H gels of relatively low Ca/Si ratio, prepared by hydration or by carbonation of a C3 S paste. The origin of the weaker, downfield peak is discussed and tentatively attributed to bridging tetrahedra of a dreierkette silicate chain structure. 相似文献
11.
Hideki Ishida Satoru Yamazaki Kaori Sasaki Yoshihiko Okada Takeshi Mitsuda 《Journal of the American Ceramic Society》1993,76(7):1707-1712
α-C2 SH can be synthesized by hydrothermal treatment of lime and silicic acid for 2 h at 200°C. When heated to 390–490°C, α-C2 SH dissociates through a two-step process to form an intermediate phase plus some γ-C2 S. This appears to be a new dicalcium silicate different from known dicalcium silicates—α, α'L , α'H , β, and γ phase—and is stable until around 900°C. At 920–960°C, all the phases are transformed to the α'L phase. The intermediate phase has high crystallinity and is stable at room temperature. 29 Si MAS NMR measurements indicate the possibility that it contains both protonated and unprotonated monosilicate anions. The intermediate phase that has passed through the α'phase at higher temperature yields β-C2 S on cooling. The intermediate phase is highly active, and completed its hydration in 1 day ( w/s = 1.0, 25°C). Among the crystalline calcium silicate hydrates with Ca/Si = 2.0, it is hillebrandite that yields β-C2 S at the lowest temperature. 相似文献
12.
Edgar A. Leone Sean Curran Margaret E. Kotun Gilbert Carrasquillo Remco van Weeren Stephen C. Danforth 《Journal of the American Ceramic Society》1996,79(2):513-517
Solid-state 29 Si NMR techniques were used to characterize laser-synthesized silicon nitride powder prepared from the reaction of silane with ammonia. When the powder is exposed to water vapor, a hydrated layer rapidly forms at the surface. A comparison of 29 Si cross polarization (CP) and Bloch decay (BD)-MAS-NMR spectra revealed differences between surface and bulk compositions. CP-NMR identified Si-NHx (x = 1, 2) species with a chemical shift of −45 ppm in the as-synthesized ( unexposed ) powder. In BD-NMR spectra, the nitride resonance is observed at −48 ppm. For the hydrated powder, CP-NMR identified additional =Si-OH ( Q3 ), =Si-(OH)2 ( Q2 ), and SiO2 ( Q4 ) species present at the surface. The CP-NMR spectra were corrected for TlpH relaxation effects and deconvoluted into individual components in order to extract quantitative measurements of the various species present. 相似文献
13.
Laurent Cormier Daniel R. Neuville Georges Calas 《Journal of the American Ceramic Society》2005,88(8):2292-2299
The anomalous behavior of the glass transition temperature ( T g ) in low silica calcium aluminosilicate glasses has been related to the structural modifications observed by neutron and X-ray diffraction. The diffraction data indicate that Al and Si are in tetrahedral sites and that Ca atoms are in distorted octahedral sites. By subtracting the correlation functions for glasses at constant SiO2 or constant Al2 O3 content, we have shown that Si and Al atoms are introduced in a different way within the glass structure. Si is present in various Q n sites, while Al resides in Q3 and Q4 sites for glasses with high CaO content and enters fully polymerized Q4 sites with increasing SiO2 or Al2 O3 content. The higher proportion of Al in Q3 positions at high CaO content yields a depolymerization of the network. The lower connectivity will contribute to a decrease of the viscosity, which may be at the origin of the decrease of T g for glasses at low silica content. 相似文献
14.
SALLY A. RODGER GEOFFREY W. GROVES NIGEL J. CLAYDEN CHRISTOPHER M. DOBSON 《Journal of the American Ceramic Society》1988,71(2):91-96
The use of cross-polarization (CP) NMR in conjunction with magic angle sample spinning (MASS) to examine the hydration reaction of tricalcium silicate (C3 S) is described. In particular the very early stages of the reaction both with and without admixtures has been studied as well as the hydration in a ball mill. The combination of CP and non-CP 29 Si NMR permits the distinction between silicate units associated with protons, i.e., in hydrated material, and those in anhydrous material. It has been found that in paste hydration there is steady formation of a small amount of hydrated monomeric silicate units during the induction period. In ball mill hydration the formation of the crystalline calcium silicate hydrate, afwillite, which contains only hydrated monomeric silicate species, can be monitored. These results are interpreted in terms of possible mechanisms for C3 S hydration. 相似文献
15.
Laurent Bonafous Catherine Bessada Dominique Massiot Jean-Pierre Coutures Bruno Le Holland Pierre Colombet 《Journal of the American Ceramic Society》1995,78(10):2603-2608
The effect on β-C2 S of two stabilizing agents, calcium sulfate and alumina, has been investigated using high-resolution 29 Si solid state NMR spectroscopy. Syntheses were achieved via the gel route, wet or dry processes. Room-temperature NMR spectra characteristics were analyzed as a function of the sintering temperature. The incorporation of Al3+ and S6+ ions, which finds expression in a noticeable line broadening, is shown to be effective above 1200°C. The 29 Si chemical shift is unchanged upon doping, suggesting a mean SiO4 tetrahedra geometry identical to that in pure β-C2 S. General trends on the structure adopted by C2 S upon Al3+ and S6+ doping are also discussed. 相似文献
16.
Stephen Kwan Judith LaRosa Michael W. Grutzeck 《Journal of the American Ceramic Society》1995,78(7):1921-1926
Strätlingite (2CaO·Al2 O3 ·SiO2 ·8H2 O) is a complex calcium aluminosilicate hydrate commonly associated with the hydration of slag-containing cements or other cements enriched in alumina. Strätlingite can coexist with the hydrogarnet solid solution [hydrogarnet (3CaO·Al2 O3 ·6H2 O)-katoite (3CaO·Al2 O3 ·SiO2 ·4H2 O)] and calcium silicate hydrate (C-S-H). Since Strätlingite is present in many blended cements, the knowledge of strätlingite's characteristic silicate anion structure and how aluminum is accommodated by the structure is important. Phase pure Strätlingite samples have been synthesized from oxides in the presence of excess water and from metakaolinite, calcium aluminate cement, CaO, NaOH, and water. The samples were characterized using X-ray diffraction (XRD), scanning electron microscopy (SEM), and thermogravimetric analysis (TGA) and then further examined using 29 Si, with and without cross-polarization (CP), and 27 Al solid-state magic angle nuclear magnetic resonance spectroscopy (MASNMR). For the most part, NMR data for these strätlingites corroborate structural information available in the literature. The aluminum atoms are both tetrahedrally and octahedrally coordinated, and the silicon atoms exist predominantly as Q2 , Q2 (1Al), and Q2 (2Al) species. The presence of alkali affects the structure of strätlingite in subtle ways, significantly reducing the AlIV /A1VI ratio. 相似文献
17.
The rate of paste hydration of 3Ca O·SiO2 (C3 S) and the effects of additions of CaCl2 , CdI2 , and CrCl3 , were studied by differential thermal analysis and thermogravimetry. X-ray analyses were used to identify the synthesized C3 S. The salts CaCl2 , CdI2 , and CrCl3 , accelerated the hydration of C3 S. The degree of hydration was estimated by the amount of Ca(OH)2 , formed, as determined by TG. 相似文献
18.
Early Hydration of Tricalcium Silicate 总被引:1,自引:0,他引:1
M. E. TADROS JAN SKALNY R. S. KALYONCU 《Journal of the American Ceramic Society》1976,59(7-8):344-347
The hydration of tricalcium silicate (C3 S) in the preacceleration stages was studied. The C3 S particles carry a positive charge during the early stages of hydration. Following a rapid hydrolysis of C3 S, calcium ions adsorbed on the Si-rich surface of C3 S particles, greatly reducing their further dissolution, thus initiating the induction period. The [Ca2+ ] and [OH- ] continue to increase at lower rates and, because Ca(OH)2 crystal growth is inhibited by silicate ions, become supersaturated with respect to Ca(OH)2 . When the supersaturation reaches a value of ∼1.5 to 2.0 times the saturation concentration, nuclei are formed, and rapid growth of Ca(OH)2 and C-S-H is initiated. These products act as sinks for the ions in solution, thus enhancing the further dissolution of C3 S. 相似文献
19.
The initial hydration processes of activated and ordinary dicalcium silicates (β-C2S) have been followed by using high resolution 29Si nuclear magnetic resonance (NMR) associated with cross-polarization and magic-angle spinning (CP/MAS) without enrichment of 29Si. The preliminary results show that the initial hydration products contain monomeric silicate hydrates and the amount of these monomeric silicate hydrates determines the hydration rate in the initial hydration period. As the hydration process goes on, the end-group of tetrahedra anions (Q1 units) appears and then gradually dominates the spectrum. 相似文献
20.
The Pore Structure of Hydrated Cementitious Compounds of Different Chemical Composition 总被引:1,自引:0,他引:1
ARNON BENTUR 《Journal of the American Ceramic Society》1980,63(7-8):381-386
The pore structure ofβ-C2 S, C3 S, and portland cement pastes was investigated using mercury porosimetry and H2 O and N2 adsorption. The β-C2 S had more total macro- and mesoporosities than C3 S and portland cement pastes of a similar degree of hydration. C3 S and portland cement pastes had similar total porosities but differed in the porosity size distribution. In the mesopore range, the various test methods gave different results. These differences are discussed on the basis of the various models proposed for cement paste. It is shown that shrinkage could be correlated with the volume of pores <0.03 μm, but not with total porosity. 相似文献