In this study, we optimized the utilization of Tunisian Aquitanian deposits from the Fortuna Formation for ceramic pigment synthesis. Samples were collected from Jebel Menchar in the Bouficha region, situated in the Northern Atlas of Tunisia. Characterized by a predominant composition of quartz and K-feldspar, Aquitanian sands were extensively investigated using X-ray diffraction (XRD), X-ray fluorescence (XRF), infrared analyses, Scanning Electron Microscopy coupled with energy dispersive spectroscopy (SEM/EDS), thermogravimetric analysis (TGA), and differential thermal analysis (DTA), serving as primary materials in the laboratory-scale production of Co-willemite and Co-olivine blue pigments. The resulting pigments demonstrated notable stability and crystalline structure, particularly when exposed to a calcination temperature of 1100 °C. The confirmation of pigment phase formation was established through XRD and FTIR analysis. Furthermore, UV–visible measurements indicated significant absorbance in the UV region. These pigments displayed semiconducting gap energies, implying potential applications in semiconducting materials or devices. Their application on both transparent and opaque glazes showcased interesting blue coloration, substantiated by measurements in the CIEL color space. Comparative analysis with commercially available equivalents revealed comparable coloring performance, suggesting the potential viability of silica sand as a source for synthesizing blue pigments with properties similar to those of established commercial alternatives. Ultimately, this research supports the use of local Aquitanian sand as a sustainable and effective raw material for the production of ceramic pigments.
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