The conversion process of quartz grains into belite clusters in portland cement clinker has been followed under isothermal heating conditions at 1400Β°C. On heating, quartz grains are surrounded by layers consisting of belite and liquid, which continue to grow thick with the progress of conversion (o
Mechanism of glass formation in portland cement clinker
β Scribed by Iwao Maki
- Publisher
- Elsevier Science
- Year
- 1979
- Tongue
- English
- Weight
- 432 KB
- Volume
- 9
- Category
- Article
- ISSN
- 0008-8846
No coin nor oath required. For personal study only.
β¦ Synopsis
In the system C3A-C~AF-SiO2-MgO, the glass formation region that is closely similar in composition to the interstitial material of portland cement clinker has been determined. The interstitial melt that exists in equilibrium with the silicates at the clinkering temperature contains a little silica. This forms clusters, which increase the viscosity of the melt and cause the latter to supercool appreciably. Crystallization of C3A and C~AF increases the concentration of clusters, which progressively inter10ck in the residual liquid, thus giving a glass on quenching. The presence of Si02 in the interstitial melt also enables the metastable formation of the orthorhombic aluminate and the oriented overgrowth of the Β£errite on the aluminate to occur through encouraging supercooling 0Β£ the melt.
π SIMILAR VOLUMES
Unequivocal phase identification of alite in portland cement clinker has been made by combined use of microscopy during heating, X-ray powder diffraction, and differential thermal analysis. Alite thus far assigned to Mlb by X-ray powder diffractometry, in reality, gives every indication of being M
Crystallization of a liquid similar to that present in Portland cement at clinkering temperatures has been studied. Its composition (in wt %) is CaO = 54.8, A~203 = 22.7, Fez03 = 16.5, Si02 = 6.0. Prolonged crystallization or slow cooling yields the equilibrium phases: C3A, ferrite close to C,AF, an
The mineralizing effect of 0.5% F-as CaF on the high-temperature reactions in the quaternary system CaO-Al$OS-Fe20S-Si02 was studied in the presence of minor amounts of MgO and K2SO4. The partitioning of fluorine between the calcium aluminate and calcium silicate phases was detennined in relation to