1 Environmental Geoscience
Sunday, 22 October 2006
8:00 AM - 12:00 PM
GEOCHEMICAL COMPOSITION OF NATURAL GRADE DIATOMITE AND ITS UTILIZATION AS ADSORPTION MEDIUM IN POLLUTION ABATEMENT
Paper number: 1-10
Program: Technical Sessions
Time: 10:30 AM – 10:45 AM
Authors
Abstract
The results indicate that the geochemical composition of the diatomite is SiO2 (84.9–85.1%), Al2O3 (8.8–9.0%), and Fe2O3 (2.5–2.8%) with a trace metal composition of Cu (3.1–3.5 ppm), Zn (4.9–5.5 ppm), Pb (0.2–0.5 ppm), and Bi (0.21–0.25 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.