
Hydraulic conductivity will be tested using variations of sediments in different proportions. (if feasible, and time permitting)
The following proportions will be tested and the results compared:
95% - sand 5% - clay
90% - sand 10% - clay
80% - sand 20% - clay
75% - sand 25% - clay
Along the Mississippi River the sediment varies in different areas. This experiment will test a few variations and retro-fit the sediment make-up to regions along the river.