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- W3048489951 abstract "This experiment is part of a larger ensemble exploring flood intermittency and delta island growth. They were conducted in the Surface Transport and Earth-surface Processes (STEP) Basin, located at the Morphodynamics Laboratory at the University of Texas at Austin.The experimental domain is 1.85 m x 2 m with a water depth of 50 mm over a 50-mm thick sediment bed. The bed is composed of the same grain size as the input sediment: fine quartz sand, with a D50 of 171 µm and a density of 2650 kg/m3.A computer controlled pump and auger feed the sediment and water (0.355 l/s at a concentration of 1:100) mixture into a bucket with an Arduino-controlled knife valve that connects to the domain inlet by a 2 inch PVC pipe. The water level in the STEP basin is maintained by a computer controlled weir, constraining water level within 1 mm of the 50 mm above the initial sediment bed height. The tank does not recirculate, and all the sediment from the flows remains in the domain during the experiments. The experiments were recorded with overhead time-lapse imagery, a photo taken every 15 seconds. The overhead images were preprocessed, correcting for lens distortions at the edge of the frames." @default.
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- W3048489951 date "2018-01-16" @default.
- W3048489951 modified "2023-09-27" @default.
- W3048489951 title "Flood Intermittency and Delta Islands" @default.
- W3048489951 doi "https://doi.org/10.5967/m0bz645x" @default.
- W3048489951 hasPublicationYear "2018" @default.
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