Effect of calcium on dissolution and precipitation reactions of amorphous silica at high alkalinity

A better understanding of silica dissolution-precipitation reactions at high pH aqueous solutions allows for promotion of favorable (e.g., pozzolanic) reactions and mitigation of deleterious (e.g., alkali-silica) reactions in concrete. In this paper, the kinetics and products of silica glass dissolution are studied as a function of solution pH, temperature, and availability of calcium. It was observed that dissolution rate versus time increases linearly with pH and reaches a maximum at pH = 14, with slower dissolution at higher alkalinities. In solutions with similarly high pH, but saturated with portlandite, glass dissolution is significantly slower. This is due to formation of a dense, low porosity, and strongly bonded C-S-H layer on the surface of glass, which serves as a barrier against diffusion of OH- and alkali ions towards the substrate glass. This protective layer forms only when Ca is abundant and portlandite saturation can be maintained on a local scale. (C) 2016 Elsevier Ltd. All rights reserved.

Published in:
Cement And Concrete Research, 87, 1-13
Oxford, Pergamon-Elsevier Science Ltd

 Record created 2016-10-18, last modified 2018-03-17

Rate this document:

Rate this document:
(Not yet reviewed)