UT Sediment Transport and Earth-surface Processes (STEP) Basin
![]() The Third in the World at UTThe unique subsidence mechanism in the STEP basin allows for investigating deltaic sedimentation under conditions of 1) fore-hinge (passive margin), 2) back-hinge (foreland basin), and 3) lateral tilting subsidence patterns. This facility will be one of only three experimental tanks in the world that provides a computer-controlled basement motion. |
Sediment, Water, and DepositionThe UT STEP basin has a size of 4 m wide, 5 m long, and 1.5 m tall. This experimental flume is designed to physically model morphodynamic and stratigraphic evolution of the fluviodeltaic system. Both 1D and 3D delta experiments can be conducted in the basin.
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Triple the Controls, Triple the Fun(+damental understanding)!
Time variations of sediment supply and sea level can be simulated during experiments along with the subsidence control. These three basinal controls are independently set by a computer and precisely monitored in the facility.
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Completed, March 2011 |
Bio-Geo Flume
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Yellowstone at Your Lab.Cascading steps developed using artificial spring water at the Laboratory! Series of test flume experiments for Carbonate sedimentation have been performed in a proto-type Bio-Geo flume facility at UIUC. Biological, chemical, and geological controls on the surface morphology and carbonate stratigraphy will be examined in both this and a new system that will be assembled at the Morphodynamics Lab, UT. Movie: Carbonate Precipitation |

