MINERALOGICAL INVESTIGATION OF THE AGGREGATE OF HYDRAULIC ROMAN MORTARS: THE AQUA TRAIANA CASE STUDY
Samples, collected at the caput aquae of Sette Botti (Trevignano Romano, Italy), located north of lake Bracciano, were investigated using a multianalytical approach. Thin sections were realized to study the mortars through optical microscopy (OM), scanning electron microscopy (SEM-EDS) and electron microprobe analysis (EMPA). Part of each sample was finely ground for X-ray powder diffraction analysis (XRPD). Additionally, the aggregate separated by the mortar was individually studied by SEM-EDS and EMPA.
The combination of different techniques has shown to be a powerful method to characterize the aggregate [3,4]. In fact, the mortars were composed mainly of natural materials with pozzolanic behavior, which gave to the lime mortar hydraulic properties, that enable it to settle also underwater. Vitruvius, in his De Architectura, listed different source’s location for the pozzolans. Thanks to the combination of different analyses, it was possible to discover the use of local tuffs from the Sabatini Volcanic District (where the caput aquae is located) but also of red pozzolan, coming from Alban Hills district.
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