| Paper No. 54-10 | ||
| Presentation Time: 10:15 AM-10:30 AM | ||
| MESOGEOCHEMISTRY: GEOCHEMICAL REACTIONS AND MASS TRANSFERS IN A NANO-SCALE PORE SPACE CONFINEMENT | ||
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WANG, Yifeng1, BRYAN, Charles1, and XU, Huifang2, (1) Repository Performance and Certification Department, Sandia National Laboratories, 4100 National Parks Highway, Carlsbad, NM 88220, ywang@sandia.gov, (2) Department of Earth & Planetary Sciences, Univ of New Mexico, Albuquerque, NM 87131 Surface chemistry and ion sorption capability of mesoporous materials are greatly influenced by a nano-scale pore space confinement. As the pore size is reduced to a few nanometers, the separation of surface acidity constants (dpK=pK2 – pK1) becomes significantly narrowed, resulting in a high surface charge density on mesopore surfaces. The change in surface acidity constants can significantly affect ion sorption onto nano-scale pore surfaces. Given the fact that nano-scale pores are widely distributed in geologic media and account for over 90% of total mineral surface area, the observed effect of nano-scale pore space confinement has important implications to many fundamental geochemical issues such as the irreversibility of ion sorption/desorption, the bioavailability of subsurface contaminants, the enrichment of trace metals in ore deposits, and the kinetics of mineral dissolution. Sandia is multi-program laboratory operated by Sandia Corporation, a Lockheed Martin Co., for the United States Department of Energy (US DOE) under Contract DE-AC04-94AL8500. | ||
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2002 Denver Annual Meeting (October 27-30, 2002)
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| Session No. 54 Geochemistry Aqueous Colorado Convention Center: C205 8:00 AM-12:00 PM, Monday, October 28, 2002 | ||
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