TDB-10-2: Fan-delta experiment performed in Tulane University Delta Basin. Experiment evolved under constant forcings of water (0.902 l/s), sediment (0.022 l/s), and sea-level rise rate 10 mm/hr). Experiment run time was 39.3 hr. Experiment used non-cohesive sediment that was 70% by volume well sorted quartz sand with a median diameter of 110 microns and 30% by volume crushed coal with a median diameter of 400 microns. Experiment performed to explore autogenic sediment transport and stratigraphy with topography monitored every 2 minutes of run time.
Wang, Y., and Straub, K.M., 2017, TDB-10-2, SEAD, http://doi.org/10.5967/M0W37TFH.
Geolocation is 29.9403477, -90.12072790000002