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Paper No. 15
Presentation Time: 8:00 AM-6:00 PM

INTERPRETING STRONTIUM ADSORPTION AT THE MINERAL-WATER INTERFACE OF NANO- AND MICRO-CRYSTALLINE TITANIUM-DIOXIDE PHASES


RIDLEY, Moira K., Department of Geosciences, Texas Tech University, Lubbock, TX 79409-1053, MACHESKY, Michael L., Illinois State Water Survey, Champaign, IL 61820 and KUBICKI, James D., Dept. of Geosciences, The Pennsylvania State University, 335 Deike Bldg, University Park, PA 16802-2712, Moira.Ridley@ttu.edu

Our understanding of the complex processes that take place at the interface between water and micro-crystalline minerals has been advanced by integrated experimental and computational studies. Surface Complexation Models (SCM) have been used to provide a framework to explicitly incorporate surface structural information with experimental studies, and to provide rigorous thermodynamic models of adsorption data.

The adsorption of Sr2+ on micro-crystalline rutile (α-TiO2) was investigated by potentiometric titrations, X-ray measurements and theoretical calculations. All data were integrated into a SCM, specifically the MUSIC model in combination with the charge distribution (CD) model. Such an all-inclusive approach has been extended to examine particle-size effects on the adsorption of Sr2+ on nano-crystalline anatase phases.

The sorption of Sr2+ was studied as a function of nanoparticle size (3–40 nm diameter), pH and loading in NaCl media at 25ºC. The adsorption of Sr2+, as indicated by the development of proton charge curves, was similar for all anatase nano-particles when normalized with respect to their pHznpc values. As anticipated, the adsorption charging curves changed as a function of surface loading, suggesting a change in the Sr2+ surface speciation. A CD-MUSIC model was used to rationalize all anatase experimental data. Furthermore, all fits were constrained by available DFT-MD simulation results for the interaction of Na+, Sr2+ and Cl- ions with the anatase (100) surface. Strontium and sodium ions adsorb as inner-sphere species, whereas Cl- electrolyte ions form outer-sphere complexes. The predominant Sr2+ surface complexes are bidentate species.

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