GEOC 26 |
| Although dissolved silicate is ubiquitous in the environment and is known to alter the reactivity of host minerals, our understanding about silicate adsorption onto iron oxide surfaces is very limited. In principle, knowledge of the silicate adsorption geometry on the hematite surface can provide a structural baseline for the interpretation of the effect of aqueous silicate and other anions on the chemical reactivity of host minerals. We report here, the three-dimensional geometry of silicate monomer adsorption on a r-plane hematite surface at circumneutral pH as determined from measurements of specular and nonspecular x-ray scattering at 90% RH and 298 K along ten crystal-truncation rods (CTR's). The scattering data provide both vertical and lateral information about the interfacial structure. Intensity changes due to silicate adsorption are evident in the (00Ls), (02Ls), (10Ls), and (11Ls) rods when compared to the clean surface scattering, and we focus on these for our analysis. |
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Physical Chemistry of Soil and Aquifer Systems: A Symposium in Honor of Garrison Sposito
1:30 PM-5:10 PM, Sunday, 10 September 2006 Moscone Center -- Room 256, Oral
Division of Geochemistry |