The effect of grinding of raw quartz on the hydrothermal reaction in CaO-SiO
2 system was investigated by using a small reaction vessel immersed in oil bath for rapid heating. Results obtained were as follows.
(1) It was found that reaction is generally accelerated by grinding, but that prolonged grinding retarded the reaction, especially, in the case of so long-time grinding as 24h, reaction hardly proceeded after 3h.
(2) The molar ratio (CaO/SiO
2) of the reacted composites was changed from 4.1 to 1.6 for unground quartz, and 0.3 to 1.9 for ground quartz.
(3) It was found that
N value of the equation, (1-
3√1-α)
N=
kt, was 1.3-2 for raw quartz, and larger than 2 for ground quartz.
(4) Ca-ion concentration in water exceeded greatly than that of silicic acid after reaction.
(5) From the results of X-ray and TG-DTA analyses, C-S-H was the only compound formed, but the textures of the hydrates were very different from each other, namely, plate or needle crystals were observed for unground quartz, and long fibrous crystals were observed for ground quartz.
From these results, it was found that the reaction took place in a different mechanism by grinding treatment, and especially, the reaction with long-time ground quartz nearly stopped in a half way. This seems likely to be due to the fact that amorphous silica produced on the surface of the ground quartz reacted rapidly, and the further reaction was inhibited by the dense layer produced in its initial stage. Therefore, the influence of amorphous silica in quartz should be taken into accout on the hydrothermal reaction in CaO-SiO
2 system.
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