Abstract
The mechanism of the formation of alkaline silicate suspensions was proposed based on the role of chemical interactions of hydroxides, silicates, carbonates, and polyphosphates of alkali metals, soluble in dispersion medium, with one another and with the surfaces of natural disperse minerals. The experimental data indicating that these interactions in alkaline silicate suspensions proceed mainly in the pH 10–11 range were summarized. Based on developed notions, practical recommendations taking into account chemical interactions were suggested for preparing the alkaline silicate suspensions with predetermined properties.
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