The CaO-A1203-CaSO4-H20 system has been investigated at 50°C and 85°C, by calculations of the equilibrium solubility surfaces of AH3, C3AH6, CH, ettringite, monosulphoaluminate and gypsum. The results indicate that monosulphoaluminate becomes a stable phase at elevated temperature. Since ettringite
Thermodynamics of the Al2O3–Al4C3 system: III. Equilibrium vapour pressures and activation energies for volatilisation
✍ Scribed by J.-M. Lihrmann
- Publisher
- Elsevier Science
- Year
- 2008
- Tongue
- English
- Weight
- 239 KB
- Volume
- 28
- Category
- Article
- ISSN
- 0955-2219
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✦ Synopsis
The present paper addresses the vapour phase in equilibrium with the compounds of the stable Al 2 O 3 -Al 4 C 3 system, between 25 • C and 1827 • C. The volatilisation of each of them into any of five gaseous species referred to as [Al x O y ], is described in terms of an activation energy and a preexponential term; for Al 2 O 3 , also sublimation is modelled on the basis of rare vapourization data. At least up to 1300 • C, the relative importance of the various [Al x O y ] derives from the activation energies necessary to form them; above 1300 • C, both activation energy and pre-exponential terms are influential. Activation energies increase with increasing ratio y/x in [Al x O y ], from approximately 365 kJ mol -1 for [Al] to about 900 kJ mol -1 for [AlO 2 ]; the effects of temperature and mole fraction Al 2 O 3 are investigated. Up to almost 1807 • C, [Al] is the predominant species regardless of carbon monoxide pressure, and thus the most likely intermediate in processes involving vapour phase reactions. Solid-vapour equilibria are illustrated in a volatility diagram at 1787 • C.
📜 SIMILAR VOLUMES
An equilibrium phase diagram has been calculated for the CaO-A1203-CaSO4-K20-H20 system at 25°C for several KOH concentrations. These KOH concentrations were chosen to relate to cement pore fluid compositions and published experimental data. In addition to the hydrates found in the CaO-A1203-CaSO4-H
The CaO-AI203-CaSO4-H20 system at 25°C has been investigatedby calcula~ons on the equilibrium solubility surfaces of AH 3, C3AH6, CH, C6AS3H x, C4ASH x and gypsum. The results are in good agreement with the previous experimental data and make it possible to define the hydrates in equilibrium with aq