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

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GRAND CHALLENGE: COMPUTATIONAL THERMODYNAMICS OF COMPLEX FLUIDS AND SOLIDSCourtesy of J. WeareFigure 27. Solubility of carbonate minerals as a function of temperature <strong>and</strong> pCO 2 . Triangles, squares <strong>and</strong> circlesrepresent experimental data; lines represent EOS predictions (Moller et al. 2005).The principal limitation to the development of accurate EOS models of the fluids encountered inthe application of energy strategies is the lack of underst<strong>and</strong>ing of the speciation (e.g., thestructure <strong>and</strong> dynamics of polyions <strong>and</strong> colloids) present in the liquid phase. For example, even<strong>for</strong> the Al system, one of the most common elements in the Earth’s crust, we have a veryincomplete underst<strong>and</strong>ing of the speciation in solution.EOS models <strong>for</strong> mixtures of aqueous electrolytes <strong>and</strong> nonaqueous mixtures also have importantapplications to CO 2 sequestration in salt <strong>for</strong>mations. Recently there has been progress in thedevelopment of Mixed-Solvent Electrolyte (MSE) models that have been shown to accuratelypredict the thermodynamics of electrolyte solutions extending to the fused salt limit <strong>and</strong> over abroad range of temperatures in aqueous-solvent mixtures. The development <strong>and</strong> application ofsuch new approaches to chemical systems involving salt brines-CO 2 mixtures could greatlyenhance our ability to predict the chemical changes in deep geologic systems of importance inCO 2 disposal. As in other areas, there is an important need <strong>for</strong> the development of more firstprinciples-basedEOS methods in this area. EOS based on a fundamental underst<strong>and</strong>ing of thespecies present in the phases are important to reduce the dependence on data <strong>and</strong> extend theextrapolation of the EOS region of reliability outside the range of the data.EOS <strong>for</strong> solids, solid solutions <strong>and</strong> absorbed phases. Current EOS <strong>for</strong> mineral systems areessentially empirical. For pure minerals this is not a problem as long as data exist to parameterizethe temperature-pressure dependence. On the other h<strong>and</strong>, even commonly encountered solidphases such as dolomite can be very complex solid solutions, with like-like <strong>and</strong> like-unlike76 <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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