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*This presentation is in Room 2.204 in the CPE Building, at 3:00 p.m. Monday, January 28, 2008*
Forced mobilization and spontaneous migration of fluids in underground formations are severely impacted by the
presence of fractures, which vastly dominate the overall conductivity of rocks. Uncertainties in the description
of transport properties in these systems often make flow predictions a difficult task. Understanding the origin
of such transport properties and their dependence on local heterogeneities and other geological features is
essential for the design of effective recovery strategies. High-resolution X-ray computed tomography allows us
to explore these heterogeneities and their impact on fluid transport with realistic detail. This presentation
shows a series of experimental findings of two-phase flow in fractured cores, with the aid of micro-scale
visualization of fluids, fracture, and rock matrix.
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