2003
DOI: 10.1016/s0008-8846(03)00224-2
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Effect of hydration temperature on the solubility behavior of Ca-, S-, Al-, and Si-bearing solid phases in Portland cement pastes

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Cited by 111 publications
(54 citation statements)
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“…The SEM micrographs show that, at early ages, the main hydration products were the ettringite (AFt) crystals and amorphous gels, such as the calcium silicate hydrate (C-S-H) or the calcium aluminum silicate hydrate (C-A-S-H) (26,(36)(37)(38). In this study, the AFt formation in the SFC cement likely complies with both Type I and Type II AFt crystals, as described by Mehta (39).…”
Section: Microstructural Analysessupporting
confidence: 69%
“…The SEM micrographs show that, at early ages, the main hydration products were the ettringite (AFt) crystals and amorphous gels, such as the calcium silicate hydrate (C-S-H) or the calcium aluminum silicate hydrate (C-A-S-H) (26,(36)(37)(38). In this study, the AFt formation in the SFC cement likely complies with both Type I and Type II AFt crystals, as described by Mehta (39).…”
Section: Microstructural Analysessupporting
confidence: 69%
“…Generally, the composition in pore solution is determined by the dissolution of the clinker phases as well as the sulfate carriers in the cement and the precipitation of the hydration products, such as ettringite, portlandite and [13][14][15][16][17][18][19][20][21][22][23][24]. During the first hours of hydration, the pore solution is dominated by high concentration ions including sodium, potassium, calcium, sulfate and hydroxide in an order of tens to hundreds millimole per liter, together with some low concentration elements such as Al, Fe and Si in an order of several tens micromole per liter.…”
Section: Pore Solution Analysismentioning
confidence: 99%
“…Figure 9 shows the measured (points) and computed (lines) pH values of the aqueous solution plotted versus the Ca/Si ratio of the solid with which the solution is in equilibrium. Computed pH values were calculated by balancing the charge of the aqueous species (e.g., CaOH + , H 2 SiO 4 2-), the distribution of which was calculated from the measured Ca and Si concentrations using a geochemical modeling program, PHREEQC [72]; the Debye-Huckel or the Davies equation was used to account for non-ideal behavior, and the ionic association constants used here are listed elsewhere [73]. For the pH values above 11.5 (the range with which we are most concerned), all values (except for several belonging to group 4) were generally within ± 0.05 of the computed values, thereby giving a selfconsistent check for the analyses of the solutions.…”
Section: Si Nmrmentioning
confidence: 99%