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Basic Research Needs for Geosciences - Energetics Meetings and ...

Basic Research Needs for Geosciences - Energetics Meetings and ...

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PRIORITY RESEARCH DIRECTION:NANOPARTICULATE AND COLLOID CHEMISTRY AND PHYSICSlarge numbers of processors, but no single processor will have high per<strong>for</strong>mance. One can takeadvantage of massively parallel computer architectures in terms of system size, but not in termsof making predictions of the system over the long time scales necessary <strong>for</strong> modelinggeochemical processes involving colloids. Also, there is need <strong>for</strong> improved accuracy insimulations from the perspectives of the data needed <strong>for</strong> models at larger scales <strong>and</strong> the ability topredict electronic structures as system size increases.Computational methods <strong>for</strong> describing particles greater than 2 nm in size (500 to 1000 atoms) donot currently have the accuracy that can be obtained <strong>for</strong> molecular systems at or below this size.This is especially true <strong>for</strong> molecular systems containing radionuclides, notably the actinides,which require relativistic treatments due to the high atomic number (Vallet et al. 2006). Methodsmust be developed to predict the electronic structure of large systems, including relativisticeffects, with the accuracy necessary <strong>for</strong> developing predictive models at the molecular tonanoscale <strong>and</strong> at higher scales. These could include new exchange-correlation functionals <strong>for</strong>Density Functional Theory <strong>and</strong> basis set-free methods as well as improvements in ab initiomolecular dynamics <strong>and</strong> solvent models to deal with long-range interactions. New approacheswill be needed <strong>for</strong> <strong>for</strong>ce-field-based methods to predict the behavior of much larger systems atlonger times, including improved <strong>for</strong>mulations <strong>for</strong> long-term dynamics, sampling of phase space,<strong>for</strong>ce fields <strong>for</strong> all atoms in the Periodic Table, <strong>and</strong> mixed electronic structure/<strong>for</strong>ce-fieldmethods based on theoretical or empirical parameters. Reactions within colloids <strong>and</strong> on theirsurfaces will require novel ways to predict solvation/desolvation <strong>and</strong> reactivity in complexsystems. Innovation is essential <strong>for</strong> the modeling of reaction kinetics, including transition states<strong>and</strong> other rare events, <strong>and</strong> thermodynamics in solution, which must include appropriate samplingof phase space <strong>for</strong> reliable predictions of entropy in complex, heterogeneous systems. Newstatistical physical approaches will be needed to predict the chemical behavior <strong>and</strong> motion oflarge colloids that may or may not be charged in solution.At the next set of scales, approaches suitable <strong>for</strong> predicting the movement of colloid-associatedcontaminants through the vadose zone <strong>and</strong> into groundwater environments rely on advances inour underst<strong>and</strong>ing of colloid mobilization, transport, <strong>and</strong> deposition within water-saturated <strong>and</strong>unsaturated porous media. Mobilization, which describes the release of colloids into pore water,is driven by fluctuations in flow <strong>and</strong> perturbations in pore water chemistry. Quantitativeinferences on mobilization rates are limited by too few observations of the phenomenon.Laboratory measurements made at the Darcy (column) scale are needed to elucidate howmobilization rates are linked to measurable properties of the porous media, pore water, <strong>and</strong>colloids. Pore-scale observations that identify mechanisms that govern mobilization are neededto guide the development of a theory <strong>for</strong> colloid release in unsaturated <strong>and</strong> saturated geologicsolids. Once mobilized, colloids move by advection <strong>and</strong> dispersion <strong>and</strong> are susceptible toremoval from the pore water (deposition) by reactions that take place near solid-water <strong>and</strong>, in thecase of unsaturated media, air-water interfaces. Knowledge of colloid transport <strong>and</strong> deposition inideal systems must be extended to account <strong>for</strong> complexities associated with real subsurfaceenvironments. In particular, the presence of organic coatings on colloid surfaces, <strong>and</strong>heterogeneity in the physical <strong>and</strong> chemical properties of the porous media, should be evaluated<strong>for</strong> their roles in influencing colloid transport <strong>and</strong> deposition. Also, parameters <strong>and</strong> models fromsmaller scales must be incorporated into the scale describing colloidal transport in naturalsystems. Thus, new <strong>and</strong> improved reactive transport approaches need to be developed to dealwith the transport of these nanoscale particles. Collectively, developments from research at the118 <strong>Basic</strong> <strong>Research</strong> <strong>Needs</strong> <strong>for</strong> <strong>Geosciences</strong>: Facilitating 21 st Century Energy Systems

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