GEOCHEMICAL COMPOSITION OF NATURAL GRADE DIATOMITE AND ITS UTILIZATION AS ADSORPTION MEDIUM IN POLLUTION ABATEMENT
The results indicate that the geochemical composition of the diatomite is SiO2 (84.985.1%), Al2O3 (8.89.0%), and Fe2O3 (2.52.8%) with a trace metal composition of Cu (3.13.5 ppm), Zn (4.95.5 ppm), Pb (0.20.5 ppm), and Bi (0.210.25 ppm). Adsorption experiments performed under similar conditions for the treatment of Pb- and Zn-contaminated wastewater indicates that the adsorption of Pb by diatomite was best described by the S-type curve isotherm, whereas the adsorption of Zn by the diatomite was indicative of the L-type curve isotherm.
Similarly, light and heavy diatomites adsorbed 42.8% and 48.8% of Pb, respectively, and 38.7% and 34.4% of Zn, respectively. The percentages of lead removal by the diatomites are expressed by the regression equations y = -0.03x + 85.72 (R2 = 0.5569) and y = -0.04x + 83.61 (R2 = 0.6466), while those of zinc are expressed by the regression equations y = 0.04x + 17.38 (R2 = 0.6499) and y = -0.06x + 61.89 (R2 = 0.0682) for heavy and light diatomites, respectively (where y = % removal by the diatomites and x = initial concentration of Pb and Zn in ppm). The diatomites have been found suitable as commercial filter media.