Influence of some mineralizers on synthesis and hydration ofβ-dicalcium silicate

Rinaldi, Domenico; Valenti, Gian Lorenzo

doi:10.1007/bf01731528

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1998

2023

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Cited by 6 publications

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“…Studies of β Ca 2 SiO 4 hydration rates [25][26][27][28][29][30][31][32][33] elu cidated the key factors that influence them. Primarily, these are the particle size distribution and specific surface area of the dicalcium silicate that undergo hydration.…”

Section: Resultsmentioning

confidence: 99%

Thermal transformations of the SCAS monolith

Chervonnyi

Чуканов

Pekov

2015

Russ. J. Inorg. Chem.

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Thermal conversions in SCAS monolith were studied in the temperature range 25-1200°C. As a result of temperature exposure, the monolith is found to undergo dehydration, dehydroxylation, and decar bonization. These processes are noticed to alter not only the amorphous component of the monolith, but also some of its crystalline phases (calcium carbonate polymorphs, melilite, and gypsum) to yield, in the ultimate product, β dicalcium silicate, which is capable of forming a binder gel under secondary hydration reactions.

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