Abstract
Zirconium (Zr) and titanium (Ti) are essential elements that are mainly sourced from the minerals zircon (ZrSiO₄) and ilmenite (FeTiO₃), rutile (TiO₂), respectively. Zircon is frequently found alongside minerals like rutile and ilmenite and is often recovered as a byproduct during their extraction. Zirconium’s properties—including a high melting point, mechanical strength, chemical stability, and corrosion resistance—make it valuable for applications in ceramics, nuclear fuel cladding, thermal insulation, catalysts, pharmaceuticals, and electronics. Titanium, similarly obtained from ilmenite, rutile (TiO₂), is highly sought after for its strength, low density, and corrosion resistance, which makes it crucial in nuclear power plant systems like piping, heat exchangers, and condensers. This study focuses on a mineralogical analysis of five beach sand samples from the coastal region of Cox's Bazar. Samples were collected from the back dune area to maximise the heavy mineral content. The overall elemental composition of the sand was measured using Wave Dispersion X-ray Fluorescence (WDXRF) and X-ray Fluorescence (XRF). In two samples (L-4 and L-5), heavy minerals such as rutile, ilmenite, zircon, magnetite, and garnet were separated using an Induced Roll Magnetic Separator (IRMS) and Electrostatic Plate Separator (ESPS). The concentration of heavy minerals in these samples was determined through a heavy liquid separation method using tetrabromoethane as the density medium. The resulting heavy mineral contents were 34.65 wt% and 47.35 wt% for samples L-4 and L-5, respectively. Portable XRF analysis of each separated heavy mineral confirmed that the separation process was effective.