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*This presentation is in Room 2.204 in the CPE Building, at 3:00 p.m. Monday, February 11, 2008*
The unsaturated zone plays an important role within the hydrologic cycle as an interface between the earth’s surface and
underlying groundwater systems. An array of important physical, chemical, and biological interfacial processes and
reactions occur in this zone over a range of spatial and temporal scales. This talk will focus mostly on the role of
wettability on water flow and distribution in unsaturated, fractionally-wet porous media. Quantitative data, extracted
from high-resolution, three-dimensional images obtained using synchrotron X-ray computed tomography, will be used to
help elucidate important pore-level processes that impact drainage, colloid transport and evaporation at larger scales.
If time permits, results will also be presented looking at the impact of fractional wettability on nonwetting phase
saturation and distribution.
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