Experiment on Bimodal Random Field

 

 



These photographs show a realization of a bimodal random permeability field.

Briefly, in work supported by the Subsurface Science Program at the U.S. Department of Energy, this flow cell was filled to mimic the structure of a second order stationary random field which had been generated on the computer. This field was studied in an effort to characterize flow and transport response in a random 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 microbes (Arthrobacter).

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.



Publications resulting from this effort included:

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.

Conwell, P.M., S.E. Silliman, and L. Zheng, “Design of a piezometer network for estimation of the variogram of the hydraulic gradient: The role of the instrument”, Water Resources Research, 33(11), 2489-2494, 1997.