2008 Joint Annual Meeting (5-9 Oct. 2008): Sorption of Dibenzo-p-dioxin by Clay Minerals: Hypotheses for Interlayer Complexation.

668-9 Sorption of Dibenzo-p-dioxin by Clay Minerals: Hypotheses for Interlayer Complexation.



Tuesday, 7 October 2008
George R. Brown Convention Center, Exhibit Hall E
Cun Liu1, Kiran Rana2, Cliff Johnston2, Hui Li1, Stephen Boyd1 and Brian Teppen1, (1)Crop and Soil Sciences, Michigan State University, East Lansing, MI 48824
(2)Department of Crop, Soil and Environmental Sciences, Purdue University, West Lafayette, IN 47907
Sorption of dibenzo-p-dioxin to smectite was studied using batch sorption technique, X-ray diffraction and Raman spectroscopy accompanied by quantum chemical calculations. Lower clay charge and interlayer cation hydration result in high affinity of dioxin, especially for Cs-saponite which effectively adsorbed dioxin from water, approaching 1 % (wt/wt). The basal spacing of Cs-saponite increased from 12 Ã… to 14.7 Ã… with dioxin loading demonstrated intercalation of dioxin into the clay interlayer. Raman spectra of dioxin associated with Cs-saponite showed significant enhancement of certain Raman lines, which were confirmed by quantum chemical calculations of simplified interlayer cation-dioxin complexations, indicated the formation of favorable electron acceptor-electron donor complexes between cation and dioxin molecule in the smectite interlayer.