Experiment on Scaled Medium



In work supported by the Subsurface Science Program at the U.S. Department of Energy, this flow cell was filled to mimic three levels of a Sierpinski Carpet in an effort to study flow and chemical transport in a structured porous medium. Results from this series of experiments include response to pumping (steady state), response of the piezometers to regional flow, response for chemical tracer tests, and response to injection of latex particles.

Instrumentation on this tank included a single inflow reservoir, three outflow reservoirs, 25 piezometers, and two fully penetrating wells. The light material in this picture is a fine sand with a hydrualic conductivity of approximately 0.057 cm/sec. The darker material is a coarser sand with a hydraulic conductivity of approximatley 0.50 cm/sec. The red color is red food coloring, used as a color tracer, moving with regional flow from the left side to the right side of this picture. The dye was added as a pulse input in the left reservoir.

Papers analyzing the results of these experiments have been presented at AGU and have appeared in two papers.

Silliman, S.E., L. Zheng, and P. Conwell, "The use of laboratory experiments for the study of conservative solute transport in heterogeneous porous media", Hydrogeology Journal, 6, 166-177, 1998.

Silliman, S.E., and S. Caswell, "Observations of measured hydraulic conductivity in two artificial, confined aquifers with boundaries", Water Resources Research, 34(9), 2203-2213, 1998.