Publication Date
Summer 2014
Degree Type
Thesis
Degree Name
Master of Science (MS)
Department
Geology
Advisor
Emmanuel Gabet
Keywords
Dry ravel, Flume experiment, Granular flow, Hillslope evolution, Multiparticle transport, Sediment transport
Subject Areas
Geology; Geomorphology
Abstract
Recent studies of sediment transport have shifted from the traditional continuum paradigm to a particle-based approach. A previous dry ravel flume experiment on single particle transport showed that the angle of repose represented a shift between friction-controlled gentle slopes dominated by local transport and inertia-driven steep slopes dominated by nonlocal transport. My flume study explored multiparticle transport and the effect of sediment volume on transport distance. The flume experiments revealed a negative relationship between sediment volume and transport distance. As sediment volume increased, inter-particle collisions increased, which led to particle jamming and a reduction in transport distance. Furthermore, a higher transition slope was required for transport to shift into the inertial regime as a result of greater sediment volume.
Recommended Citation
Kuoch, Alan, "Examination of Multiparticle Transport as a Function of Slope and Sediment Volume" (2014). Master's Theses. 4472.
DOI: https://doi.org/10.31979/etd.qfwj-e94e
https://scholarworks.sjsu.edu/etd_theses/4472