In this study, the hydration reaction between cement and volcanic glass powder (VG)and its hydrates were clarified, assuming the use of VG as a substitute for silica fume (SF), which is often used in ultra-high-strength concrete. Furthermore, the relationship between the pore structure formed by the hydrates and the compressive strength development was also examined. As a result, the following findings were obtained. The total pore volume of the cement hardened body mixed with VG reached a minimum and the compressive strength peaked when the admixture ratio was 25%. On the other hand, in the case of SF, the total pore volume was at its minimum and the compressive strength peaked when the admixture ratio was 20%. As the admixture ratio of both VG and SF increased, the amount of C-S-H formation increased and the pore volume decreased due to the pozzolanic reaction, resulting in an increase in compressive strength. The peak admixture ratio of the pozzolanic reaction was 25% and 20%, respectively. The C-S-H produced when the VG admixture ratio was below 30% had a higher percentage of high-density C-S-H compared to SF, and the percentage of low-density C-S-H increased rapidly when the admixture ratio reached 30%. The amount of C-S-H produced when the VG admixture ratio was 30% increased over that at the VG admixture ratio was 25%, but the amount of pores increased. However, the compressive strength when the VG admixture ratio was 30% was similar to that at the VG admixture ratio was 25%. Based on the analysis of pore size distribution volume and C-S-H density, it was inferred that this was caused by an increase in the amount of pores in the gel porosity region due to the formation of more low-density C-S-H.
View full abstract