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

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APPENDIX 1: TECHNICAL PERSPECTIVES RESOURCE DOCUMENT<strong>and</strong> gas applications, this uncertainty is neither characterized initially nor propagated throughsuccessive elements of work flows because it is not critical to current operations. New datacommonly are not integrated with prior data in a fashion as to reduce or manage the initialuncertainty. Various approaches, including stochastic inversion (Ramirez et al. 2005) providetools <strong>and</strong> approaches to address this task; however, they require large computational resources<strong>and</strong> expert capability, <strong>and</strong> have not been broadly applied to common subsurface operations.Improved technology development <strong>and</strong> deployment in uncertainty rendering <strong>and</strong> managementwould dramatically improve the accuracy of site-specific work <strong>and</strong> the ability of operators toselect monitoring <strong>and</strong> characterization tools that would reduce uncertainty.Fracture systems <strong>and</strong> geomechanicsFracture networks may be critical components to geological carbon sequestration targets <strong>for</strong>several reasons:1. They can play a substantial, sometimes dominant, role in the hydrological flow field2. They can represent potential migration fast paths through cap-rocks <strong>and</strong> along fault networks3. Their transmissivity may be dynamic, responding to both pressure transients <strong>and</strong> chemicaldisequilibriaThe response of existing fracture networks to pressure <strong>and</strong> stress transients are of specialimportance in saline <strong>for</strong>mations where the pre-injection pressure is likely to be hydrostatic. Inaddition, overpressures generated by the CO 2 injections may generate new local fracture systemswith different properties. In unmineable coal units, the rock volumes swell in the presence ofCO 2 , closing fractures (cleats) <strong>and</strong> dramatically reducing injectivity. Fracture orientation <strong>and</strong>density have been successfully inferred from observations of seismic anisotropy from shearwavesplitting (e.g., Li 1997), but seismic characterization of fracture permeability remains a keyresearch objective <strong>for</strong> the oil <strong>and</strong> gas industry. In rendering fracture networks <strong>and</strong> their processresponse, substantial uncertainties remain in fracture orientation, length, transmissivity, <strong>and</strong>response to stress.Mineral chemical kineticsMineral carbonation has been regularly observed in natural analog systems, <strong>and</strong> laboratoryexperiments provide thermodynamic <strong>and</strong> kinetic constraints <strong>for</strong> some key minerals or mineralassemblages. These constraints greatly impact the accuracy <strong>and</strong> precision of complex reservoirsimulations (e.g., Johnson et al. 2005). At least three important technical needs remain:1. A more comprehensive suite of kinetic <strong>and</strong> equation-of-state data sets, particularly aimed atthe small fraction of the rock volume with rapid reaction kinetics (e.g., metal oxides <strong>and</strong>hydroxides; Kharaka et al. 2006)2. An improved theoretical <strong>and</strong> experimental basis <strong>for</strong> determining the reactive surface areawithin a rock3. The effects of trace (co-contaminant) gases on phase equilibria <strong>and</strong> kineticsSimulation <strong>and</strong> modelingShort- <strong>and</strong> long-term modeling is central to many aspects of planning, operational control,analysis, risk assessment, <strong>and</strong> site decommissioning. At present, simulation <strong>and</strong> modeling are theprimary tools <strong>for</strong> providing qualitative or quantitative assessments of the long-term fate of CO 2Appendix 1 • 22<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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