INVESTIGATION OF MINERALOGICAL AND GEOCHEMICAL PROPERTIES OF SILICATE-RICH MINE WASTE FROM A KYANITE MINE IN CENTRAL VIRGINIA
Fifteen representative samples were collected in April of 2008. X-ray diffraction indicates that four minerals are dominant: quartz, muscovite, hematite, and kyanite. Muscovite composes approximately 3 to 5 percent of the waste, is uniform in chemical composition and is Ti-bearing. DCP analysis of major elements resulted in SiO2 (87.89-90.99 wt %), Al2O3 (6.75-7.74 wt %), Fe2O3 (1.13-1.28 wt %), K2O (0.36-0.60 wt %). Other major elements such as TiO2, P2O5, CaO, Na2O, MgO, and MnO were present at concentrations < 1.0 wt% or were below detection limits. ICP-MS analysis for trace elements of particular concern showed concentrations of Ag (0.05-1.7 ppm), As (0.01-0.36 ppm), Ba (177.28-218.97 ppm), Cr (6.83-8.40 ppm), Cu (12.38-37.61 ppm), Hg (0.02-3.46 ppm), Ni (4.95-14.35 ppm), Pb (18.42-31.51 ppm), Sb (0.06-2.68 ppm), Sn (4.03-6.82 ppm) Tl (0.01-0.73 ppm), V (52.54-57.36 ppm), and Zn (0.57-5.53 ppm). Se and Cd had concentrations below detection. Other trace elements detected but of less concern include Be, Rb, Sr, and Zr.
Mineralogy combined with hydraulic conductivity measurements (0.025 to 0.061 cm/s) suggests the waste is suitable for use in constructed wetlands. Bulk chemical data however indicates there are some elements of concern, although the concentrations of many are relatively low and the solubility of these components has not been determined. Muscovite is of a quality such that it may be recycled. Kyanite is of low concentration and occurs in textures not conducive to recycling. Results of this investigation suggest environmental and economic gains may be achieved by recycling this waste stream.