Experimental analysis of pore-scale flow and transport in porous media |
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Affiliation: | 1. Environmental Programs Directorate, Lawrence Livermore National Laboratory, University of California, Livermore, California 94550, USA;2. Battelle, Pacific Northwest Laboratories, Richland, Washington 99352, USA;3. Sandia National Laboratories, Livermore, California 94550, USA;1. Department of Chemistry Ångström Laboratory, Uppsala University, Box 523, SE 75120 Uppsala, Sweden;2. Department of Physics, University of Nairobi, P.O. Box 30197-00100, Nairobi, Kenya;3. Department of Engineering Sciences, Nanotechnology and Functional Materials, Uppsala University, Box 534, SE 75120 Uppsala, Sweden;4. Labratoary of photomolecular science, École Polytechnique Fédérale de Lausanne, SB-ISIC-LSPM, Chemin des Alambics, Station 6, CH G1 523, CH-1015 Lausanne, Switzerland;1. Dr., Department of Applied Geology, Western Australian School of Mines, Curtin University, GPO Box U1987, WA, Australia;2. Dr., Department of Applied Geology, Western Australian School of Mines, Curtin University, GPO Box U1987, WA, Australia;3. Dr., Department of Applied Geology, Western Australian School of Mines, Curtin University, GPO Box U1987, WA, Australia |
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Abstract: | ![]() A novel, non-intrusive fluorescence imaging technique has been used to quantitatively measure the pore geometry, fluid velocity, and solute concentration within a saturated, three-dimensional porous medium. Discrete numerical averages of these quantities have been made over a representative volume of the medium and used to estimate macroscopic quantities that appear in conventional continuum models of flow and transport. The approach is meant to illustrate how microscopic information can be measured, averaged, and used to characterize medium-scale processes that are typically approximated constitutively. The experimental system consisted of a clear, cylindrical column packed with clear spherical beads and a refractive index-matched fluid seeded with fluorescent tracer particles and solute dye. By illuminating the fluid within the column with a scanning planar laser beam, details of flow and concentration within the pore spaces can be quantitatively observed, allowing for three-dimensional, dimensional, time dependent information to be obtained at good resolution. In time dependent information to be obtained at good resolution. In the current experiment, volumetrically averaged velocities and void-to-volume ratios are first compared with bulk measurements of fluid flux and medium porosity. Microscopic measurements of concentration are then used to construct cross-sectionally averaged profiles, mean breakthrough curves, and direct measurements of the dispersive flux, velocity variance, and concentration variance. In turn, the dispersive flux measurements are compared with mean concentration gradients to provide a basis for confirming the Fickian dispersion model and estimating dispersion coefficients for the medium. Coefficients determined in this manner are compared with others based upon traditional length-scale arguments, mean breakthrough analyses, and curve fits with numerical simulations. |
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