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

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PRIORITY RESEARCH DIRECTION:DYNAMIC IMAGING OF FLOW AND TRANSPORTFigure 40. Illustration of available tracers <strong>and</strong> the current “age gap” that exists in dating the age of fluids in geologicreservoirs. Courtesy of K. Solomon, University of Utah (personal communications). Modified from L.N. Plummer,USGS (personal communications; see also Plummer et al. 1993).The interaction of physical fields with fluid-filled rocksAdvances in the basic underst<strong>and</strong>ing of how physical fields (i.e., acoustic <strong>and</strong> electromagneticwaves) interact with subsurface materials <strong>and</strong> fluids are needed <strong>for</strong> better inversion ofgeophysical data. Seismic <strong>and</strong> electromagnetic data are rich in in<strong>for</strong>mation, but the ability to mapthis geophysical in<strong>for</strong>mation into physical, chemical <strong>and</strong> biological processes is hampered bygaps in underst<strong>and</strong>ing of how these fields interact with the subsurface. For example, the state ofstress in the subsurface changes the propagation of seismic signals, but the direct relationbetween the velocity <strong>and</strong> attenuation of seismic waves with the microscale properties of fluidfilledfractured rocks is poorly understood. The problem becomes more challenging whenincluding interactions of rock heterogeneity <strong>and</strong> fabric with pore fluid pressure <strong>and</strong> anisotropicstress fields. An improvement in the fundamental knowledge of how microscale responses tostress fields influences wave propagation needs to be developed <strong>and</strong> would enable inversion ofdata to determine the stress state in the field. Similar questions arise regarding seismic <strong>and</strong>electromagnetic response to changes in temperature. Advanced experiments using, <strong>for</strong> example,X-ray spectroscopy, will improve underst<strong>and</strong>ing of the microscale physical properties thatcontrol geophysical responses. Links between many geophysical responses (e.g., seismicattenuation, travel time, compressive-to-shear-wave ratio, electrical <strong>and</strong> magnetic fields) <strong>and</strong>rock/fluid properties have yet to be fully understood <strong>and</strong> exploited. Coupled models <strong>for</strong> flow128 <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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