“…Moreover, the reduction with maturing age in the volume of gel and capillary pores for most of the series analyzed would be due to the progress of slag and clinker hydration [22,52] and the pozzolanic reactions of fly ash [17,18], which would produce a progressive formation of solid phases, partially closing the microstructure in the long term. The higher volume of finer pores generally observed for series with fly ash and slag, regardless of the aggregate used, could be related to the reactivity of these additions, and this result would be in keeping with other authors [17,18,[53][54][55]. In the case of slag, it has hydraulic activity [22,52,56], so it is capable to react directly with the setting water, forming new solids, which would fill the existing pores, thus reducing the volume of larger voids in the microstructure.…”