Abstract
Pure tricalcium silicate and portland cement pastes made with variable water solid ratios were cured at 20 °C for 1 to 24 months. It was found that even after the hydration reaction had been terminated the pastes exhibited gradual changes in their specific surface area as determined by N 2 and H 2O adsorption and in pore size distribution as determined by Hg porosimetry.
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