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2 were nearly identical. 3 exhibit longitudinal dispersivities 2 to 3 times larger that the uniform size particles. 36 On the other hand Sternberg et al. (1996) obtained the opposite result. 2 em. 0 em. 163 mm. The beads were packed into the column in four different ways, two homogeneous (all bead 1, all bead 2) and two heterogeneous (114 length of one bead followed by 1/2 length of the other bead followed by 1/4 length of the first bead, and its opposite permutation). The measurement consists of monitoring the change in concentration of a chloride tracer (KCl) as a function of time and position as a low concentration solution is displaced by a high concentration solution.
Some of these are: The assembly of the evaluated sheets into a velocity map of the complete measuring space requires delicate alignment when virtual images are observed. Translation of the CCD-camera behind the hologram to change the position ofthe reconstructing aperture, shifts the observation field accordingly, which must be corrected by an appropriate tilt of the camera. Alternatively, it will be easier to assemble sub-volumes in real-image space which, however, requires a conjugate complex reconstructing wave of high fidelity.
To obtain the flow field inside a porous medium in three-dimensions a 3D imaging technique must be adopted to detect tracer particle movements. , 1994); (b) defocusing (Willert and Gharib, 1992); (c) holographic (Hinsch and Himichs, 1996) and (d) stereoscopic (Maas, 1996). Saleh et al. (1992), Cenedese and Viotti (1996) and Rashidi et al (1996) present applications of 2D imaging-based techniques to obtain velocities, trajectories, dispersion tensor components, and spatial averaged properties. Other non-invasive techniques based on Positron Emission Tomography (PET) (Khalili et al.